Search results

...5/a095/0001/0200/0221.htm Capillary pressure] in D. Morton-Thompson and A. M. Woods, eds., Development Geology Reference Manual: [http://store.aapg.org/

...amu.edu/publications/tnotes/tn30/tn30_2.htm Ocean Drilling Program Texas A&M University article]

| author = Grant M. Skerlec ...a 100-m column of oil might leak if the column increased to [[length::101 m]].

...and is what is displayed on a sonic log, usually in units of μs/ft or μs/m. It is also seen as ''delta t'' or ''Δt''.

...in the Paraná basin, which displays large-scale sets of cross strata (1-30 m; [[:file:Botucatu_1.jpg|Figure 1]]), formed in a desert environment similar

[[File:Vápeč_od_Horn%C3%AD_Poruby.jpg|thumb|300px|Vápeč Hill (955 m), Strážovské vrchy Mountains, District Ilava, Slovakia. Highest part of

| author = Grant M. Skerlec ...[[hydrocarbon column]]. Seals can be extremely thin—less than [[length::1 m]] thick that seal individual hydrocarbon [[accumulation]]s. There are also

* Burger, H., R., Hamill, M., 1976, Petrofabric analysis of the Dry Creek Ridge anticline, Montana: Geo * Burkhard, M., 1993, Calcite twins, their geometry, appearance and significance as stres

| author = Grant M. Skerlec ...me=ch10r27>England, W., A., Mackenzie, A., S., Mann, D., M., Quickley, T., M., 1987, The movement and entrapment of petroleum fluids in the subsurface:

...era as indicators of organic carbon flux, in M. A. Kaminski, S Geroch, and M. A. Gasiński, eds., Proceedings of the Fourth International Workshop on Ag

| author = Grant M. Skerlec ...nsylvania, SEALS International, 3948 p.</ref><ref name=ch10r74>Skerlec, G. M., 1997b, Atlas of fault seal behavior in the Gulf Coast: Franklin, Pennsylv

| author = Grant M. Skerlec ...tion Research Company internal report.</ref><ref name=ch10r71>Skerlec, G., M., 1990, SEALS: A short course for risking top seal and fault seal: Franklin

# Determine ''m'' using the table of values. ==Step 3: Determine ''m''==

| author = Grant M. Skerlec ...G Bulletin, vol. 81, no. 6, p. 897–917.</ref><ref name=ch10r74>Skerlec, G. M., 1997, Atlas of fault seal behavior in the Gulf Coast: Franklin, Pennsylva

:<math>\mbox{R} = {-}(\mbox{k} \times \mbox{A/m} \times [(\mbox{P}_{\rm grad} + \mbox{P}_{\rm c}) - \rho_{\rm hc} \times \m * R = rate of migration (m³/sec)

| author = Grant M. Skerlec ...carbon in the field in the Tar Springs Formation reservoir is [[length::29 m]] [[depth::(95 ft]]).

| author = John M. Armentrout ...ld: Pliocene-Pleistocene, northwestern Gulf of Mexico ''in'' P. Weimer and M. J. Link, eds., Seismic facies and sedimentary processes of submarine fans

...D. A., 2002, Volcanology and facies architecture of flood basalts, ''in'' M. A. Menzies, S. L. Klemperer, C. J. Ebinger, and J. Baker, eds., Magmatic r ...magma types:<ref name=Peate_1992>Peate, D. W., C. J. Hawkeswort, and M. S. M. Mantovani, 1992, Chemical stratigraphy of the Parana lavas (South America)

...evidence.<ref name=ch21r47>Van Wagoner, J. C., Mitchum, R. M., Campion, K. M., Rahmanian, V. D., 1990, Siliciclastic Sequence stratigraphy in Well Logs, ! Sequence order || Cycle frequency, m.y. || Thickness, m || Stratigraphic name

...essure]] (''P''_b ) at the depth of the measured pressure (P_m ) from the measured pressure: #*:<math>P_{\rm b} = P_{\rm m} - P_{\rm hydrostatic}</math>

...ula <math>\text{V} = \text{A} \times \text{T} \times \text{Y} \times \text{M}</math>, where: #* ''M'' = migration efficiency

| author = Grant M. Skerlec ...trolled instead by fault-dependent leak points.<ref name=ch10r3>Allard, D. M., 1993, Fault leak controlled trap fill, rift basin examples (abs.), in J.

:<math>\mbox{S}_{\rm w} = \left(\frac{1}{\Phi^{\rm m}} \times \frac{\mbox{R}_{\rm w}}{\mbox{R}_{\rm t}}\right)^{\rm 1/n}</math> * m = cementation exponent, which varies from 1.7 to 3.0 but normally is 2.0

| author = John M. Armentrout ...field: Pliocene–Pleistocene, northwestern Gulf of Mexico, in P. Weimer and M. J. Link, eds., Seismic Facies and Sedimentary Processes of Submarine Fans

...ut too tight to produce. Between these are [[length::30 ft]] [[depth::(8.5 m]]) of mesoto macroporous sandstone (flow units 1-4). * M = medium grained

...p>13</sup>C values. From Bordenave and Burwood;<ref name=ch08r2>Bordenave, M. L., and R. Burwood, 1990, [[Source rock]] distribution and [[maturation]] ...g, H. M., M. A. Rooney, M. B., Toon, G. E. Claypool, M. A. Rooney, and R. M. Squires, 1994, [http://archives.datapages.com/data/bulletns/1994-96/data/p

:<math>\mbox{P}_{\rm G} = [\rho_{\rm m} \times (1 - \phi) \times \mbox{d}] + [\rho_{\rm w} \times \phi \times \mbo * ρ_m = weighted average of grain (mineral) density (sandstone and shale =

...sequence stratigraphy, in Wilgus, C. K., Hastings, B. S., Posamentier, H. M., Van Wagoner, J., Ross, C. A., Kendall, G. C. St. C., eds., Sea-Level Chan ...er et al.<ref name=ch21r47>Van Wagoner, J. C., Mitchum, R. M., Campion, K. M., Rahmanian, V. D., 1990, Siliciclastic Sequence stratigraphy in Well Logs,

...ello, A. G., L. J. Bauer, T. A. Battista, P. W. Mueller, M. S. Kendall and M. E. Monaco, 2009, Shallow-Water Ben­ thic Habitats of St. John, U.S. Virgi

...recoverable reserves of about 300 million bbl of oil (48 × 10⁶ m³). The main pay interval is the lower part of the Midale, called ...Subtle seals and fluid-flow barriers in carbonate rocks, in J. C. Dolson, M. L. Hendricks, and W. A. Wescott, eds., Unconformity Related Hydrocarbons i

| author = John M. Armentrout ...rative fractionation reported by Thompson<ref name=ch04r95>Thompson, K. F. M., 1987, Fractionated aromatic petroleums and the generation of gas-condensa

| author = Grant M. Skerlec ...hea et al..<ref name=ch10r68>Shea, W., T., Schwalbach, J., R., Allard, D., M., 1993, Integrated rock-log evaluation of fluvio-lacustrine seals, in Ebank

| author = John M. Armentrout ...Group (Paleocene), central Texas coastal plain, in R. D. Winn, Jr., and J. M. Armentrout, eds., Turbidites and Associated Deep-Water Facies: WEPM Core W

...sured temperature, found on the log header. If only mud resistivity (R_m) is given, convert it to R_mf as explained below. ==Converting r_m to r_mf==

| author = John M. Armentrout ...e=ch04r29>Dow, W. G., M. A. Yukler, J. T. Senftle, M. C. Kennicutt, and J. M. Armentrout, 1990, Miocene oil source beds in the East Breaks basin, Flex-T

| Amplitude (m) || High (50–100) || Moderate (20–50) || Low (1–20) ...ds, in Read, J., F., Kerans, C., Webber, L., J., Sarg, J., F., Wright, F., M., eds., Milankovitch Sea-level Changes, Cycles, and Reservoirs on Carbonate

...gram; (bottom left) m/z 217 fragment in the mass spectrometer; (top right) m/z 218 fragment. Copyright: Unocal.]] ...meter, while the top right chromatogram shows those compounds that give an m/z 218 fragment. The 217 and 218 mass chromatograms are very similar because

...age in exploration: the spectrum of seepage styles], in D. Schumacher, and M. A. Abrams, eds., Hydrocarbon Migration and Its Near-Surface Expression: [h ...try as an exploration tool in the South Caribbean], in D. Schumacher, and M. A. Abrams, eds., Hydrocarbon Migration and Its Near-Surface Expression: [h

...the updip change in pore throat sizes could account for 280–890 ft (95–298 m) of oil column. The column height shown from producing wells at Weyburn and ...]), then the total column could not exceed [[length::300 ft]] [[depth::(90 m]]).

...ed. For example, suppose a potential [[source rock]] unit is [[length::100 m]] thick. What was the average calculated from: * 10 samples, [[length::10 cm]] thick, taken every 10 m

* Antonellini, M., and A. Aydin, 1995, [http://archives.datapages.com/data/bulletns/1994-96/ * Finkbeiner, T., C. A. Barton, and M. D. Zoback, 1997, [http://archives.datapages.com/data/bulletns/1997/12dec/1

...memoir66/11/0139.htm Migration a view from the top], in D. Schumacher, and M. A. Abrams, eds., Hydrocarbon Migration and Its Near-Surface Expression:[ht ...l Explorationists Bulletin, vol. 8, p. 1–17.</ref><ref name=ch18r1>Abrams, M. A., 1992, Geophysical and geochemical evidence for subsurface hydrocarbon

| 0.1 and 100 m/year | 0.001 and 1 m/year

.../ref> Reymond and Stampfli<ref name=ch13r10>Reymond, B., A., Stampfli, G., M., 1994, Sequence stratigraphic interpretation of 3D seismic data offshore L

...rbon seepage in near-surface marine sediments], in Schumacher, D., Abrams, M., A., eds., Hydrocarbon Migration and Its Near-Surface Expression: [http://

| author = John M. Armentrout ...ock, although Taylor and Armentrout<ref name=ch04r93>Taylor, G. S., and J. M. Armentrout, 1990, Rock geochemistry and relationships to produced oils fro

| author = Grant M. Skerlec ..., p. 840–850.</ref><ref name=ch10r68>Shea, W. T., J. R. Schwalbach, and D. M. Allard, 1993, Integrated rock-log evaluation of fluvio-lacustrine seals, i

...ne]] interbedded with bentonite, sandstone, and silt.<ref>Burtner, R., and M. Warner, 1984, Hydrocarbon generation in Lower Cretaceous Mowry and Skull C ...in, Wyoming, Montana, South Dakota, and Nebraska, ''in'' P. D. Warwick and M. D. Corum, eds., Geologic framework for the national assessment of carbon d

| author = Grant M. Skerlec ...</ref> and Vavra et al.<ref name=ch10r87>Vavra, C. L., J. G. Kaldi, and R. M. Sneider, 1992, [http://archives.datapages.com/data/bulletns/1992-93/data/p

...t has moved past some critical portion of the fault plane.<ref>Skerlec, G. M., 1996, Risking fault seal in the Gulf Coast (abs.): AAPG Annual Convention

...erence is in the depth to the onset of oil generation, where [[depth::1000 m]] separates the top of the oil windows of these two kerogen types. ! Present-day depth, m, Type II

...n Circular 40 (Li et al.<ref name=Lietal>Li, Peng, M. E. Ratchford, and D. M. Jarvie, 2010, Geochemistry and thermal maturity analysis of the Fayettevil

...hether the strain exceeds the seal ductility.<ref name=Skerlec>Skerlec, G. M., 1999, [http://archives.datapages.com/data/specpubs/beaumont/ch10/ch10.htm

| author = Grant M. Skerlec ...)90004-2</ref> and clay mineralogy<ref name=ch10r14>Corbett, K., Friedman, M., Spang, J., 1987, [http://archives.datapages.com/data/bulletns/1986-87/dat

.... S. de Alvarenga, E. L. Dantas, M. M. Pimentel, C. G. de Oliveira, and L. M. de Araújo, 2006, Shrimp U–Pb zircon dating and palynology of bentonitic

...e=ch05r12 /> These porosities are those that would be expected at 700-1200 m in normally pressured rock sections. ...s.<ref name=ch05r7>Gaarenstroom, L., R. A. J. Tromp, M. C. de Jong, and A. M. Brandenburg, 1993, Overpressures in the Central North Sea: implications fo

| author = Grant M. Skerlec ...(600 psi).<ref name=ch10r40>Jev, B. I., C. H. Kaars-Sijpesteign, M. P. A. M. Peters, N. W. Watts, and J. T. Wilkie, 1993, [http://archives.datapages.co

...k-correlations_fig8-40.png|Figure 1]] illustrates this trend. It shows the m/z 217.2 mass chromatograms of three oils from central Myanmar in successive ...panes and moretanes in a heavily biodegraded oil (bottom), revealed in the m/z 177 mass chromatogram. From Volkman et al.;<ref name=ch08r57>Volkman, J.

| author = John M. Armentrout ...smic stratigraphy, Pliocene–Pleistocene, Gulf of Mexico, in P. Weimer, and M. H. Link, eds., Seismic Facies and Sedimentary Processes of Submarine Fans

...ociation of facies.<ref name=ch21r47>Van Wagoner, J. C., R. M. Mitchum, K. M. Campion, and V. D. Rahmanian, 1990, Siliciclastic Sequence stratigraphy in ...th field, southwestern USA, in J. F. Read, L. J. Weber, J. F. Sarg, and F. M. Wright, eds., Milankovitch Sea-Level Changes, Cycles, and Reservoirs on Ca

| author = Grant M. Skerlec ...es, including siltstones, marls, and chalks.<ref name=ch10r71>Skerlec, G., M., 1990, SEALS: A short course for risking top seal and fault seal: Franklin

| author = John M. Armentrout ...on in the GOM basin. Copyright: Armentrout<ref name=Arm1993>Armentrout, J. M., 1993, Relative seal-level variations and fault-salt response: offshore Te

...tle seals and fluid-flow barriers in carbonate rocks, ''in'' J. C. Dolson, M. L. Hendricks, and W. A. Wescott, eds., Unconformity related hydrocarbons i

| author = Grant M. Skerlec ...orrection factor that ranges from 15–250 psi.<ref name=ch10r78>Sneider, R. M., and G. Bolger, 1993, Estimating seals from wireline logs of clastic seals

...f sampling design and density in target recognition], in D. Schumacher and M. A. Abrams, eds., Hydrocarbon Migration and Its Near-Surface Expression: [h ...for geochemical surveys may vary from 500–1,000 m at one extreme to 50–100 m at the other. Sampling along geochemical grids is recommended for small exp

....htm Natural-gas hydrates: Resources of the twenty-first century?], ''in'' M. W. Downey et al., eds., Petroleum provinces of the twenty-first century: [ ...st gas hydrates accumulations are in rough accord at about 20,000 trillion m³ (706,200 tcf).</blockquote>

| author = E. P. Mason, M. J. Bastian, R. Detomo, M. N. Hashem, A. J. Hildebrandt ...Pass 62 field, lying 50 km southeast of the Mississippi River delta in 100 m of water ([[:file:Mth14ch04f01.jpg|Figure 1]]), was discovered in 1965. It

...as an exploration tool in the South Caribbean], in Schumacher, D., Abrams, M., A., eds., Hydrocarbon Migration and Its Near-Surface Expression: [http:// ...ocarbon exploration: one company's experience], in Schumacher, D., Abrams, M. A., eds., Hydrocarbon Migration and Its Near-Surface Expression: [http://s

...Paleozoic Total Petroleum System. From Pollastro.<ref>Pollastro, R. M., D. M. Jarvie, R. J. Hill, & C. W. Adams, 2007, [http://archives.datapages.com/da ...</ref> Montgomery,<ref>Montgomery, S. L., D. M. Jarvie, K. A. Bowker, & R. M. Pollastro, 2005, [http://archives.datapages.com/data/bulletns/2005/02feb/0

| author = John M. Armentrout ...APG Studies in Geology No. 1], p. 1–10.</ref><ref name=ch04r70>Mitchum, R. M., Jr., and J. C. Van Wagoner, 1990, High-frequency sequences and eustatic c

...Subtle seals and fluid-flow barriers in carbonate rocks, in J. C. Dolson, M. L. Hendricks, and W. A. Wescott, eds., Unconformity Related Hydrocarbons i

...ations are at least [[length::250 m]].y. old—maybe as old as [[length::300 m]].y. ...cements in the reservoir.<ref name=ch11r22>Lee, M., J. L. Aronson, and S. M. Savin, 1985, [http://archives.datapages.com/data/bulletns/1984-85/data/pg/

..., Subtle seals and fluid-flow barriers in carbonate rocks, in J.C. Dolson, M.L. Hendricks, and W.A. Wescott, eds., Unconformity Related Hydrocarbons in

! Type || Single Scene Coverage (km) || Resolution (m) * Insley, M. W., F. X. Murphy, D. Naylor, and M. Critchley, 1996, The use of satellite imagery in the validation and verifi

| author = Grant M. Skerlec * ''h'' = thickness of the hydrocarbon column, ft or m

...e rock beginning to generate hydrocarbons at a depth of approximately 2200 m. Copyright: Ungerer et al.;<ref name=Ungerer1991>Ungerer, P., P. Forbes, an ...ginning to generate hydrocarbons at a depth of approximately [[depth::2200 m]].

...l.<ref>[https://oilgas.ogm.utah.gov/pub/Publications/Reports/Prod/Field/?C=M;O=D Field Production Reports, Utah]</ref> | colspan = 4 | Structural closure, 800 ft (270 m); oil column, 450 ft (150 m)

...nd proposed working model of surface geochemical exploration, in Davidson, M. J., ed., Unconventional Methods in Exploration for Petroleum and Natural G ...n exploration: the spectrum of seepage styles], in Schumacher, D., Abrams, M., A., eds., Hydrocarbon Migration and Its Near-Surface Expression: [http://

| author = John M. Armentrout ...Group (Paleocene), central Texas coastal plain, in R. D. Winn, Jr., and J. M. Armentrout, eds., Turbidites and Associated Deep-Water Facies: WEPM Core W

| author = John M. Armentrout ...e 1-B oils<ref name=ch04r96>Thompson, K. F. M., M. C. Kennicutt II, and J. M. Brooks, 1990, [http://archives.datapages.com/data/bulletns/1990-91/data/pg

* Watson, M. P., A. B. Hayward, D. N. Parkinson, and Z. M. Zhang, 1987, [http://www.sciencedirect.com/science/article/pii/02648172879 ...tic reconstruction of China and its neighboring regions, in A, Yin, and T. M. Harrison, eds., The Tectonic Evolution of Asia: Cambridge, Mass., Cambridg

...bon-induced alteration of soils and sediments], in Schumacher, D., Abrams, M., A., eds., Hydrocarbon Migration and Its Near-Surface Expression: [http:// ...ometrics: post-survey drilling results, in Davidson, M., J., Gottlieb, B., M., eds., Unconventional Methods in Exploration for Petroleum and Natural Gas

...., 1190/1., 1440255</ref> and controlled source<ref name=ch16r3>Goldstein, M. A., and D. W. Strangway, 1975, Audio-frequency magnetotellurics with a gro ...orm. This signal is transmitted into a grounded dipole typically 600–1,200 m (2,000–4,000 ft) long. The transmitter is normally located 3–6 km (2–

| author = John M. Armentrout ...w York, Springer-Verlag, p. 137–170.</ref><ref name=ch04r9>Armentrout, J., M., 1996, High-resolution sequence biostratigraphy: examples from the Gulf of

| author = John M. Armentrout ...gin]] has been influenced by several factors:<ref name=ch04r26>Coleman, J. M., and H. H. Roberts, 1991, Mississippi River depositional system: model for

| author = John M. Armentrout ...from the ''Glob alt'' sandstones and the ''Glob alt'' sandstone 200-ft (60-m) isopach.

....</ref><ref>Fulljames, J. R., L. J. J. Zijerveld, R. C. M. W. Franssen, G. M. Ingram, and P. D. Richard, 1996, Fault seal processes, in Norwegian Petrol

| author = Grant M. Skerlec ...tests, well [[stimulation]]s, and subsurface waste disposal.<ref>Evans, D. M., 1966, The Denver area earthquakes and the Rocky Mountain Arsenal disposal

| author = John M. Armentrout ...ual Research conference, p. 142–145.</ref><ref name=ch04r10>Armentrout, J. M.,and J. F. Clement, 1990, Biostratigraphic calibration of depositional cyc

| author = A. M. Sam Sarem ...ure number|3}}Vertical sweep efficiency (coverage) as a function of WOR, ''M'', and permeability variation (''V''_DP), where WOR = 5.<ref name

* ''R''_m = 2.5 Ω-m at [[temperature::70&deg;F]] * ''R''_mf = 2.0 Ω-m at [[temperature::70&deg;F]]

| author = Grant M. Skerlec

| author = John M. Armentrout ...c stratigraphy, Pliocene–Pleistocene, Gulf of Mexico, in Weimer, P., Link, M., H., eds., Seismic Facies and Sedimentary Processes of Submarine Fans and

...t prolific unconventional reservoirs outside of North America. At over 500 m thick with multiple stacked organic-rich intervals, the Vaca Muerta has gar ...highest potential for unconventional development<ref name=Zbrsk>Zborowski, M., 2018, [https://jpt.spe.org/how-does-vaca-muerta-stack-vs-us-shale-data-te

| author = Grant M. Skerlec ...ction Research Company internal report.</ref><ref name=ch10r71>Skerlec, G. M., 1990, SEALS: A short course for risking top seal and fault seal: Franklin

| author = John M. Armentrout ...w York, Springer-Verlag, p. 137–170.</ref><ref name=ch04r9>Armentrout, J., M., 1996, High-resolution sequence biostratigraphy: examples from the Gulf of

...</ref> quoted widths in excess of 40 km (25 mi) and thicknesses up to 1200 m (3937 ft) for the very large braided river systems (Table 1). These form in ...m (3-3937 ft); most < 60 m (197 ft); common range 5-60 m (16-197 ft) || 50 m-1300+ km (164 ft-808+ mi); many > 1 km (0.62 mi); common range 0.5-10 km (0

| author = John M. Armentrout ...within the same structure<ref name=ch04r86>Schanck, J. W., C. C. Cobb, and M. L. Ivey, Jr., 1988, East Breaks 160 field on the offshore Texas shelf edge

...500 m (5,000 ft), the thickness of the layer needs to be approximately 150 m (500 ft) or more. Low-resistivity layers are more easily delineated than hi

| author = Grant M. Skerlec ...ediments near Lilstock, U.K., shows a gouge zone approximately [[length::5 m]] thick. The gouge consists predominantly of ductile shales and marls as we

...zy, M., B. Steer, F. Abu-Shadi, M. Schlorholtz, J. Mika, J. C. Dolson, and M. Zinger, 1996, Gulf of Suez rift basin sequence models--Part B: Miocene seq

...bb, A. Yin, T. M. Harrison, J. Célérier, G. E. Gehrels, C. E. Manning, and M. Grove, 2011, Cenozoic tectonic history of the Himachal Himalaya (northwest ...: Geology vol. 13.10, pp. 679-682.</ref><ref>Beaumont, C., R. A. Jamieson, M. H. Nguyen, and B. Lee, 2001, Himalayan tectonics explained by extrusion of

...field, southwestern U.S.A., in J. F. Read, L. J. Weber, J. F. Sarg, and F. M. Wright, eds., Milankovitch Sea-Level Changes, Cycles, and Reservoirs on Ca ...wedge trap: Lower Cretaceous Cutbank Sandstone, Montana, in J. C. Dolson, M. L. Hendricks, and W. A. Wescott, eds., Unconformity-Related Hydrocarbons i

..., such as Van Wagoner et al.<ref>Van Wagoner, J. C., H. W. Posamentier, R. M. Mitchum, P. R. Vail, J. F. Sarg, T. S. Loutit, and J. Hardenbohl, 1988, An

| author = John M. Armentrout

...from less than 6 to 140 m (Figure 2), and its depth ranges from 0 to 1585 m, with the deepest part located in southern Illinois[2, 3]. The New Albany S 2. Strąpoć, D., M. Mastalerz, A. Schimmelmann, A. Drobniak, and N.R. Hasenmueller, 2010, Geoc

| author = Grant M. Skerlec ...sylvania, SEALS International, 3948 p.</ref><ref name=ch10r74>Skerlec, G., M., 1997b, Atlas of fault seal behavior in the Gulf Coast: Franklin, Pennsylv

...The larger the degree of fracturing, the closer the value of ''m'' is to ''m''_f. These models permit quantification of fracture porosity.

| author = Grant M. Skerlec ..., p. 1502–1509, DOI: 10.2118/19299-PA.</ref><ref name=ch10r74>Skerlec, G., M., 1997b, Atlas of fault seal behavior in the Gulf Coast: Franklin, Pennsylv

...Subtle seals and fluid-flow barriers in carbonate rocks, in J. C. Dolson, M. L. Hendricks, and W. A. Wescott, eds., Unconformity Related Hydrocarbons i

...worlds, in Read, J. F., Kerans, C., Webber, L. J., Sarg, J. F., Wright, F. M., eds., Milankovitch Sea-level Changes, Cycles, and Reservoirs on Carbonate ...ty]] greatest in grainy upper parts of sequences and thicker [[length::(10 m]] or more) than greenhouse sequences

| author = John M. Armentrout ...y specific geographic unit in a depositional basin.<ref name=ch04r37>Gary, M., R. McAfee, Jr., and C. L. Wolf, 1974, [https://www.agiweb.org/pubs/glossa

| author = John M. Armentrout ...a and the present. From Armentrout;<ref name=Armentrout1996>Armentrout, J. M., 1996, High-resolution sequence biostratigraphy: examples from the Gulf of

...ls and rocks from the central Adriatic Basin (Italy and Yugoslavia), in J. M. Moldowan, P. Albrecht, and R. P. Philp, eds., Biological markers in sedime ...iloil-and-oilsource-rock-correlations_fig8-44.png|Figure 2]] shows sterane m/z 217 mass fragmentograms of an immature rock extract (bottom left), a hydr

| author = Grant M. Skerlec ...rstanding of the variables that control [[seal]]s<ref name=ch10r19>Downey, M., W., 1984, [http://archives.datapages.com/data/bulletns/1984-85/data/pg/00

* Halbouty, M. T., ed., 1992, Giant Oil and Gas Fields of the Decade: AAPG Memoir 54, 526 * Davison, I., Bosence, D., Alsop, G. I., Al-Aawah, M. H., 1996, Deformation and sedimentation around active Miocene salt diapirs

...mical stability. From Loucks et al.;<ref name=Loucks1984>Loucks, R. G., M. M. Dodge, and W. E. Galloway, 1984, [http://archives.datapages.com/data/specp ...her et al.<ref name=ch09r60>Stonecipher, S., A., Winn, R., D. Jr., Bishop, M., G., 1984, [http://archives.datapages.com/data/specpubs/sandsto2/data/a059

...of environments. Targets ranged in depth from 1,000–15,000 ft (300–4,4600 m) and covered the full spectrum of [[trap]] styles; survey areas ranged from

| author = John M. Armentrout ...EPM Special Publication 42, p. 125–154.</ref><ref name=ch04r70>Mitchum, R. M., Jr., and J. C. Van Wagoner, 1990, High-frequency sequences and eustatic c

:<math>\mbox{S}_{\rm w}{}^{\rm n} = \frac{\mbox{R}_{\rm w}}{(\Phi^{\rm m} \times \mbox{R}_{\rm t})}</math> * m = cementation exponent, which varies from 1.7 to 3.0 but normally is 2.0

| m³/h-m | m³/h-m

...ield, southwestern U.S.A., in J. F. Read, L. J. Weber, J. F. Sarg, and F. M. Wright, eds., Milankovitch Sea-Level Changes, Cycles, and Reservoirs on Ca ...{{figure number|1}}Planktonic and foraminiferal data taken on a 30-ft (9.1-m) interval show abundance peaks crossing a sharp log break from a thin carbo

...15 m of the well, with a strong density difference. (4) Missed pay about 1 m from the well; the density difference is very pronounced. From Bayer;<ref n ...rofracturing the reservoir. In Case #4 the missed pay is about [[length::1 m]] from the well, and the density difference is very pronounced. Such pay zo

...g normal faults geometries at depth: theory and examples], in Roberts, A., M., Yielding, G., Freeman, B., eds., The Geometry of Normal Faults: Geologica ...stratigraphic framework of the northern Gulf Coast continental margin], in M. P. A. Jackson, D. G. Roberts, and S. Snelson, eds., Salt Tectonics: A Glob

...If so, then the total height of this combined column is about 600 ft (180 m). Could rocks of the porous mudstone facies act as a lateral seal for this * GOR = 100 CFG/BO (18 m³ gas/m³ oil) (probably low estimate)

...tle seals and fluid-flow barriers in carbonate rocks, ''in'' J. C. Dolson, M. L. Hendricks, and W. A. Wescott, eds., Unconformity related hydrocarbons i

| author = Grant M. Skerlec ...APG Bulletin, vol. 50, no. 2, p. 363–374.</ref><ref name=ch10r3>Allard, D. M., 1993, Fault leak controlled trap fill, rift basin examples (abs.), in J.

| author = Grant M. Skerlec ...tion Research Company internal report.</ref><ref name=ch10r71>Skerlec, G., M., 1990, SEALS: A short course for risking top seal and fault seal: Franklin

...ijks Geologie Dienst, vol. 45, p. 103–109.</ref><ref name=ch17r59>Lorente, M., A., 1990b, Textural characteristics of organic matter in several subenvir

...e than 17.2 million m³ (108 million bbl) of oil and 2.7 billion m³ (94 billion ft³) of gas from upper Miocene, deep-wat ...voirs in the basin and have contributed about 15% of more than 1.9 billion m³ (12.3 billion bbl) of oil produced in the area since 1864. Beca

| author = John M. Armentrout

High-amplitude (60 to over [[length::100 m]]), high-frequency (fourth- and fifth-order; see [[Hierarchy of sequences]] ...ds, in Read, J., F., Kerans, C., Webber, L., J., Sarg, J., F., Wright, F., M., eds., Milankovitch Sea-level Changes, Cycles, and Reservoirs on Carbonate

...drill pipe added to the drill string (i.e., every [[length::30 ft]], or 9 m) and represents an amalgamated sample of the rocks penetrated in that inter ...drill pipe added to the drill string (i.e., every [[length::30 ft]], or 9 m). However, the geologist can specify a different interval if necessary.

...h as [[length::1 km]], the line spacing in 3-D surveys can be [[length::50 m]] or less. This dense coverage requires an accurate knowledge of shot and r ...izes are 25 by [[length::25 m]] for land surveys and 12.5 by [[depth::37.5 m]] for marine surveys.

| author = E. P. Mason, M. J. Bastian, R. Detomo, M. N. Hashem, A. J. Hildebrandt .../a012/0001/0250/0289.htm Prudhoe Bay&mdash;A ten year perspective], ''in'' M. T. Halbouty, ed., Giant oil and gas fields of the decade: [http://archives

* Valderrama, M., H., Nielsen, K., C., McMechan, G., A., 1996, [http://archives.datapages.c * Telford, W., M., Geldart, L., P., Sheriff, R., E., 1990, Applied Geophysics: Cambridge, Ca

| author = Grant M. Skerlec ...ge from 15–72 dynes/cm.<ref name=ch10r87>Vavra, C. L., J. G. Kaldi, and R. M. Sneider, 1992, [http://archives.datapages.com/data/bulletns/1992-93/data/p

...D., 1994a, Non-compositional controls on diagenetic processes, in Wilson, M., D., ed., [[Reservoir quality]] Assessment and Prediction in Clastic Rocks ...findings mainly on North Sea sandstones, Scherer<ref name=ch09r53>Scherer, M., 1987, [http://archives.datapages.com/data/bulletns/1986-87/data/pg/0071/0

...source-receiver spacing is longer, on the order of [[length::10 ft]] (3.05 m); and (3) the receiver is commonly an array consisting of four to twelve ph ...ntified in a full waveform acoustic log.<ref name=pt07r6>Cheng, C. H., and M. N. Toksöz, 1981, Elastic wave propagation in a fluid-filled borehole and

...ennicutt and Brooks;<ref name=KennicuttBrooks1988>Kennicutt, M. C., and J. M. Brooks, 1988, Surface geochemical exploration studies predict API gravity

...ximately at the western margin. From Mello et al.;<ref name=ch08r30>Mello, M. R., P. C. Gaglianone, S. C. Brassell, and J. R. Maxwell, 1988a, Geochemica ...ource-rock-correlations_fig8-50.png|300px|thumb|{{figure number|3}}Typical m/z 191 mass chromatograms for group I (top) and group IV (bottom) oils from

...Craton (Fig. 1). Sedimentary infill is interpreted to be as thick as 9000 m mostly constituted of siliciclastic sedimentary and minor volcanic rocks of ...the Kyalla Formation (Roper Group), constrained by a cut-off depth of 400 m below surface<ref>Williams, B., 2019, Definition of the Beetaloo Sub basin:

...odified from Van Wagoner et al.;<ref>Van Wagoner, J. C., R. M. Mitchum, K. M. Campion, and V. D. Rahmanian, 1990, Siliciclastic Sequence Stratigraphy in ...Late Cenozoic of the Gulf of Mexico. From Mitchum et al.;<ref>Mitchum, R. M., P. R. Vail, and J. B. Sangree, 1977, [http://archives.datapages.com/data/

| author = John M. Armentrout ...c stratigraphy, Pliocene–Pleistocene, Gulf of Mexico, in Weimer, P., Link, M., H., eds., Seismic Facies and Sedimentary Processes of Submarine Fans and

| author = John M. Armentrout ...ew York, Springer-Verlag, p. 137–170.</ref><ref name=ch04r9>Armentrout, J. M., 1996, High-resolution sequence biostratigraphy: examples from the Gulf of

...basin.<ref name=ch21r47>Van Wagoner, J., C., Mitchum, R., M., Campion, K., M., Rahmanian, V., D., 1990, Siliciclastic Sequence Stratigraphy in Well Logs ...field, southwestern U.S.A., in J. F. Read, L. J. Weber, J. F. Sarg, and F. M. Wright, eds., Milankovitch Sea-Level Changes, Cycles, and Reservoirs on Ca

| author = John M. Armentrout

! Duration, m.y. ! Typical thickness, m

...Subtle seals and fluid-flow barriers in carbonate rocks, in J. C. Dolson, M. L. Hendricks, and W. A. Wescott, eds., Unconformity Related Hydrocarbons i

...S., E. Calais, E. Saria, C. Hartnady, J.-M. Nocquet, C. J. Ebinger, and R. M. Fernandes, 2008, [http://web.ics.purdue.edu/~ecalais/projects/ear/Stamps_e ...aries.<ref name=Calaisetal2006a>Calais, E., C. J. Ebinger, C. Hartnady, J. M. Nocquet, 2006, Kinematics of the East African Rift from GPS and earthquake

..., as depicted on the right of [[:Image:Charles-l-vavra-john-g-kaldi-robert-m-sneider_capillary-pressure_1.jpg|Figure 1c]]).<ref name=Journel_1989>Journe ...terpolated, as on the left of [[:Image:Charles-l-vavra-john-g-kaldi-robert-m-sneider_capillary-pressure_1.jpg|Figure 1b]]. In addition, the transfer fun

| author = Grant M. Skerlec

| author = John M. Armentrout Armentrout<ref name=ch04r9>Armentrout, J., M., 1996, High-resolution sequence biostratigraphy: examples from the Gulf of

1.Song, M., 2018, The exploration status and outlook of Jiyang depression: China Petr 5.Ma, Y., M. Fan, Y. Lu, H. Liu, Y. Hao, Z. Xie, L. Peng, X. Du, and H. Hu, 2017, Middl

...mber|2}}Income tax calculations for example development well. All amounts $M. | Capitalized IDCs, $M || 0.000 || || || || || || ||

...e-House Worlds: SEPM Short Course 35, 79 p.</ref><ref name=ch21r52>Wilson, M. D., ed., 1994, Reservoir quality Assessment and Prediction in Clastic Rock

* Paterson, M. S., 1987, Problems in the extrapolation of laboratory rheological data: Te ...ue of laboratory tests on rocks, in Carter, N. L., Friedman, M., Logan, J. M., Stearns, D. W., eds., Mechanical Behavior of Crustal Rocks: American Geop

...ozoic geochronology and chronostratigraphy, in W. A. Berggren, D. V. Kent, M.-P. Aubry, and J. Hardenbol, eds., Geochronology, Time Scales, and Global S ...nce and diversity: implications for sequence stratigraphic analysis, in J. M. Armentrout, and B. F. Perkins eds., Sequence Stratigraphy as an Exploratio

| author = Grant M. Skerlec

...2 km). From Fritz et al.<ref name=Fritzetal_2012>Fritz, R. D., P. Medlock, M. Kuykendal, and J. L. Wilson, 2012, [http://archives.datapages.com/data/spe

...nd formally designated in 2005<ref name=Scherer_et_Lavina_2005>Scherer, C. M. S., and E. L. Lavina, 2005, Sedimentary cycles and facies architecture of ...tological synthesis of the Gondwana formations of Uruguay. In: CRESWELL, M.M. & VIELLA, P. (eds) Gondwana Rotterdam, A. A. Balkema, New York, p. 47-52.<

| author = Sedat Inan, Mahdi A. AbuAli, Ahmed M. Hakami ...<ref name=Cantrelletal2014>Cantrell, D. L., P. G. Nicholson, G. W. Hughes, M. A. Miller, A. G. Bhullar, S. T. Abdelbagi et al., 2014, [http://http://arc

...chardson, 1985, Geochemistry of greater Ekofisk crude oils, in Thomas, B., M., eds., Petroleum geochemistry in exploration of the Norwegian Shelf: Londo ...150/0195.htm Ekofisk: first of the giant oil fields in western Europe], in M. T. Halbouty, ed., Giant Oil and Gas Fields of the Decade 1968–1978: AAPG

* H_w = height above P (ft or m) * Z = height (elevation) of P above a datum (ft or m)

| [[Dipmeter]] || 6 || 22 || √ || √ || √ || √ || M || × || × || √ || <3000 ...rginally acceptable conditions, NR = not recommended, NA = not applicable, M = with special modifications.</sub><br>

* Reynolds, A., D., Simmons, M., D., Bowman, M., B., J., Henton, J., Brayshaw, A., C., Ali-Zade, A., A., Guliyev, I., S.,

| author = Grant M. Skerlec

| author = John M. Armentrout ..., modified from Gross et al.<ref name=ch04r40>Gross, O. P., K. C. Hood, L. M. Wenger, and S. C. Harrison, 1995, Seismic imaging and analysis of source a

...HRZ, when present, has a resistivity of 5 Ω-m or greater and peaks at 11 Ω-m in Pike County, MS (John et al., 1997; Lu et al., 2015). The HRZ ranges up Borrok, D.M., Yang, W., Wei, M., and Mokhtari, M., 2019. Heterogeneity of the mineralogy and organic content of the Tuscaloo

| author = John M. Armentrout ...From Armentrout;<ref name=ch04r8 /><ref name=Armentrout1996>Armentrout, J. M., 1996, High-resolution sequence biostratigraphy: examples from the Gulf of

| author = John M. Armentrout ...flow regimes of the Louisiana Gulf Coast above a depth of 20,000 ft (6096 m). From Hanor and Sassen.<ref name=Hanorandsassen_1990>Hanor, J. S., and R.

...r2015b>Lazar, O. R., K. M. Bohacs, J. Schieber, J. H. S. Macquaker, and T. M. Demko, 2015b, Mudstone primer: Lithofacies variations, diagnostic criteria ...Lzr2015b />; Bohacs et al.<ref> Bohacs, K. M., J. D. Ottmann, O. R. Lazar, M. Dumitrescu, R. Klimentidis, J. Schieber, R. Montelli, C. Liu, and J. Shamr

...ween the injected fluids and the oil in place (see “[[Waterflooding]]”). ''M'' is usually stated in terms of the [[Relative permeability]] of a fluid ph :<math>M = (k_{\rm rw}/\mu_{\rm w})/(k_{\rm ro}/\mu_{\rm o})</math>

..., S., 1985, Geochemistry of the greater Ekofisk crude oils, in Thomas, B., M., eds., Petroleum Geochemistry in the Exploration of the Norwegian Shelf: L ...up>) || (&times; 10⁹ ft³) || (&times; 10⁹ m³)

...rosity]] and 10 md [[permeability]], then the bottom [[length::75 ft]] (20 m) of the trap will produce both oil and water in a long transition zone. Com

| author = John M. Armentrout

...the U.S. Gulf Coast. From Loucks et al.;<ref name=Loucks>Loucks, R. G., M. M. Dodge, and W. E. Galloway, 1984, [http://archives.datapages.com/data/specp Scherer<ref name=ch09r53>Scherer, M., 1987, [http://archives.datapages.com/data/bulletns/1986-87/data/pg/0071/0

| author = John M. Armentrout ...smic stratigraphy, Pliocene–Pleistocene, Gulf of Mexico, in P. Weimer, and M. H. Link, eds., Seismic Facies and Sedimentary Processes of Submarine Fans

...f> <ref>M. Wilt, D. L. Alumbaugh, H. F. Morrison, A. Becker, K. H. Lee and M. Deszcz-Pan, "Crosswell electromagnetic tomography: System design considera Equation (2) H_z = (-M)/(4πr^3 ) e^{(-ik_b r)} (1+ik_b r-k<sub>b</sub

...<ref name=Turneretal1987>Turner, C. C., J. M. Cohen, E. R. Connell, and D. M. Cooper, 1987, A depositional model for the South Brae oilfield, in J. Broo ...recognized (Bentley and Smith, 2008<ref name=Bentleyandsmith2008>Bentley, M. R., and S. A. Smith, 2008, Scenario-based reservoir modelling: The need fo

...d_1992>Reed, B., 1992, [[Offshore rigs]], ''in'' D. Morton-Thompson and A. M. Woods, eds., Development geology reference manual: AAPG Methods in Explora ...2000 m (1640 and 6562 ft).<ref name=Weimerandslatt_2004>Weimer, P., and R. M. Slatt, 2004, Petroleum systems of deep-water settings: Society of Explorat

...c Chart] as its guide to formal chronostratigraphy.<ref name=ICS>Cohen, K. M., S. C. Finney, P. L. Gibbard, and J.-X. Fan, 2013, The ICS International

| author = Grant M. Skerlec ...faults in the exploration and production of North Sea hydrocarbons], in A. M. Roberts, G. Yielding, and B. Freeman, eds., The Geometry of Normal Faults:

...pressure'', which is often quoted in pressure units of bars at [[length::1 m]] (bar meters). Another measure of the performance of the array is the ''pe ...put two, three, or four groups in a cable ''section'' (75 to [[length::100 m]] long), which is a unit with connectors at each end. When a section is dam

| author = John M. Armentrout ...a. Modified. Copyright: Armentrout;<ref name=Armentrout1993>Armentrout, J. M., 1993, Relative seal-level variations and fault-salt response: offshore Te

...e, 1985, Carbonate cementation--a brief review, in N. Schneidermann and P. M. Harris, eds., Carbonate CEments :SEPM Special Publication 36, p. 79-95.</r

| author = John M. Armentrout

| author = Grant M. Skerlec

...name=Johnsonetal_1999>Johnson, R. C., R. A. Crovelli, B. G. Lowell, and T. M. Finn, 1999, An assessment of in-place gas resources in the low-permeabilit ...., National Petroleum Council, 222 p.</ref> || ICF<ref name=ICF_1990>Haas, M. R., 1990, Impact of improved technology on potential reserves of tight gas

| author = John M. Armentrout ...sland South Addition in the GOM basin. From Armentrout;<ref>Armentrout, J. M., 1993, Relative seal-level variations and fault-salt response: offshore Te

| author = Grant M. Skerlec

| author = John M. Armentrout ...ch has on deposition or erosion is enhanced.<ref name=ch04r70>Mitchum, R., M., Jr., Van Wagoner, J., C., 1990, High-frequency sequences and eustatic cyc

| author = John M. Armentrout ...smic stratigraphy, Pliocene–Pleistocene, Gulf of Mexico, in P. Weimer, and M. H. Link, eds., Seismic Facies and Sedimentary Processes of Submarine Fans

| '''Editor''' || 1 M || Wiki user account || Yes || Edit || Anyone who goes through the editor

| author = Stefan M. Luthi | 800 ft/hr (245 m/hr)

...ntia.<ref name=Derbyetal_2012>Derby, J. R., R. J. Raine, A. C. Runkel, and M. P. Smith, 2012, [http://archives.datapages.com/data/specpubs/memoir98/CHAP ...name=Palmer_1981>Palmer, A. R., 1981, Subdivision of the Sauk sequence, in M. E. Taylor, ed., Short papers for the 2nd International Symposium on the Ca

* Coward, M. P., T. S. Daltaban, and H. Johnson, eds., Structural Geology in Reservoir * Wiltschko, D. V., K. P. Corbett, M. Friedman, and J.-H. Hung, 1991, Predicting fracture connectivity and inten

| author = John M. Armentrout ...ied from Gross et al.<ref name=Grossetal_1995>Gross, O. P., K. C. Hood, L. M. Wenger, and S. C. Harrison, 1995, Seismic imaging and analysis of source a

| >30 m | 2–30 m

| author = Grant M. Skerlec ...anging wall]] and [[footwall]] cutoffs.<ref name=ch10r86>Van Wijhe, D. H., M. Lutz, and J. P. H. Kaasschieter, 1980, The Rotliegend in the Netherlands a

oiloil-and-oilsource-rock-correlations_fig8-23.png|{{figure number|1}}m/z 217 mass fragmentograms from two oils showing quite different distributio ...ples deposited where marine organisms lived.<ref name=ch08r32>Moldowan, J. M., W. K. Seifert, and E. J. Gallegos, 1985, [http://archives.datapages.com/d

...on of Geologists Symposium, p. 81–96.</ref>, <ref name=ch09r39>Muller, M., M., Coalson, E., B., 1989, Diagenetic and petrophysical variations of the Dak

| author = Charles L. Vavra, John G. Kaldi, Robert M. Sneider [[File:charles-l-vavra-john-g-kaldi-robert-m-sneider_capillary-pressure_1.jpg|thumb|300px|{{figure_number|1}}Effects of

* Reservoirs less than [[length::3 m]] thick ...ds, in Read, J., F., Kerans, C., Webber, L., J., Sarg, J., F., Wright, F., M., eds., Milankovitch Sea-level Changes, Cycles, and Reservoirs on Carbonate

....<ref name=ch05r7>Gaarenstroom, L., R. A. J. Tromp, M. C. de Jong, and A. M. Brandenburg, 1993, Overpressures in the Central North Sea: implications fo

| author = John M. Armentrout ...hydrocarbon fluids to the reservoir facies.<ref name=ch04r69>Mitchum, R., M., Jr., 1985, Seismic stratigraphic expression of submarine fans: AAPG Memoi

...ox{L}(\mbox{dPb}_{n}\times \mbox{Q}_{n}) \times \, (\mbox{WOB}_{o} - \mbox{M})(\mbox{RPM}_{o}) \times \mbox{L}(\mbox{dPb}_{o} \times \mbox{Q}_{o})</math * M = threshold weight, or the WOB needed to cause formation failure, generally

...9-452.</ref>; Ramos et al.<ref name=Ramosetal_2006>Ramos, E., M. Marzo, J. M. de Gibert, K. Tawengi, A. Khoja, and N. D. Bolatti, 2006, [http://archives The Ghadamis intracratonic sag basin contains up to 5200 m (17,060.4 ft) of Paleozoic through Mesozoic clastics. The estimated recover

...th Brae Field, Blocks 16/07a, 16/07b, UK North Sea, in J. G. Gluyas and H. M. Hichens, eds., United Kingdom oil and gas fields commemorative millennium ...structural spill point to the west. Depth contours shown are in 100 ft (30 m) TVD increments. Area of map is shown in [[:file:M115CH10FG01.jpg|Figure 1]

| author = Dale M. Short ...e in “shot holes” ranging in depth from 10 to [[length::300 ft]] (3 to 100 m) and primacord in trenches covered by a few inches of soil. However, in som

...o note the structural high apparent in Devonian strata about [[length::800 m]] (2500 ft) above [[basement]] in the West Campbell field, conveniently nes ...ere mapped about [[length::500 m]] (1600 ft) above basement and show 30–90 m (100–300 ft) of displacement. Note the high degree of correlation between

| author = Denise M. Stone

...00 ft|200]], [[depth::500 ft|500]], or [[depth::1000 ft]] (61, 152, or 305 m) to record the checkshot, or vertical traveltime, at successively shallower ...be moved no more than [[length::50 ft|50]] to [[length::100 ft]] (15 to 30 m) when recording a VSP. Specifically, the vertical distance between successi

...if any (the example shown in [[:Image:Charles-l-vavra-john-g-kaldi-robert-m-sneider capillary-pressure 1.jpg|Table 1]] uses the constant dollar concept | Gross Income, $M || 0.000 || 1576.075 || 864.968 || 474.705 || 260.503 || 142.978 || 78.468

...on, J. Yeh, P. Calderon, R. Barba, M. Rodriquez, J. Castillo, M. H. Holtz, M. Sanchez ...rn Venezuela,<ref>Audemard, F. E., I. Azpiritxaga, P. Bauman, A. Isea, and M. Latreille, 1985, Marco geologico del Terciario de la Faja Petrolifera del

...l clays in a sandstone. After Wilson and Pittman.<ref name=ch09r68>Wilson, M. D., Pittman, E. D., 1977, Authigenic clays in sandstones: recognition and ...he, 1985, Carbonate cementation—a brief review, in N. Schneidermann and P. M. Harris, eds., Carbonate Cements: SEPM Special Publication 36, p. 79–95.<

| author = John G. Jkaldi, Catherine M. Gibson-Poole, Tobias H. D. Payenberg ...by Working Group III of the IPCC (B. Metz, O. Davidson, H. C. de Connick, M. Loos, and L. A. Meyer, eds): New York, Cambridge University Press, 442 p.<

Hover over the quantity to see feet: [[depth::2300 m]].

...much faster than the rate of structural growth.<ref name=ch11r15>Hubbert, M., K., 1953, [http://archives.datapages.com/data/bulletns/1953-56/data/pg/00 ...y gathering areas<ref name=ch11r8>England, W., A., Mann, A., L., Mann, D., M., 1991, [http://archives.datapages.com/data/specpubs/geochem1/data/a037/a03

...08r41>Peters, K. E., J. M. Moldowan, A. E. Kontorovich, B. J. Huizinga, J. M. Moldowan, and C. Y. Lee, 1994, [http://archives.datapages.com/data/bulletn

| author = John M. Armentrout

...2.</ref><ref name=ch21r38>Read, J. F., Kerans, C., Sarg, J. F., Wright, F. M., 1995, Milankovitch Sea-Level Changes, Cycles, and Reservoirs on Carbonate ...eters thick that were deposited between sea level cycles that lasted 0.5–5 m.y. During the 1980s, a finer resolution of stratigraphic analysis developed

...J. A., 1993, Oil to source rock correlation. Concepts and case studies, in M. H. Engel, and S. A. Macko, eds., Organic Geochemistry: New York, Plenum Pr ...L., S. Schouten, J. S. Sinninghe Damste, J. W. de Leeuw, D. Merrit, and J. M. Hayes, 1992, The combined application of organic sulphur and isotope geoch

Lagoe<ref name=ch17r54>Lagoe, M. B., 1987, The stratigraphic record of sea-level and climatic fluctuations ...Group, UK sector, North Sea, in Morton, A., C., Haszeldine, R., S., Giles, M., R., Brown, S., eds., Geology of the Brent Group: Geological Society Speci

...thern Sicily. From Ocampo et al.;<ref name=ch08r35>Ocampo, R., A. Riva, J. M. Trendel, J. Riolo, H. J. Callot, and P. Albrecht, 1993, Petroporphyrins as

| author = Jeremy M. Boak ...\alpha_{i-1} + \left[ (\alpha_{i} - \alpha_{i-1}) \times \frac{(\mbox{MD}_{m} - \mbox{MD}_{i-1})}{(\mbox{MD}_{i} - \mbox{MD}_{i-1})} \right]</math>

...lson, M. D., 1994a, Non-compositional controls on diagenetic processes, in M. D. Wilson, ed., Reservoir Quality Assessment and Prediction in Clastic Roc

...ype II-S (French et al.<ref name=French>French, K. L., J. E. Birdwell, and M. D. Lewan, 2020, Trends in thermal maturity indicators for the organic sulf ...n, J. A. Pitman, M. S. Varonka, J. Chenault, W. H. Orem, P. B. McMahon, A. M. and Jubb, 2020, Origin and geochemistry of formation waters from the lower

...nct zones that represent two ends of a spectrum:<ref name=ch09r35>Longman, M. W., 1980, [http://archives.datapages.com/data/bulletns/1980-81/data/pg/006 ...tion by boring algae occurs at the sediment–water interface to [[length::1 m]] below the interface.<ref name=ch09r35 /> Sediments deposited in lagoons,

| author = John M. Armentrout

...mage source: Abdul-Hamid M. Emwas, Zeyad A. Al-Talla, Yang Yang, and Najeh M. Kharbatia. (March 2012). Gas Chromatography–Mass Spectrometry of Bioflui ...can be performed in either full scan mode, to cover either a wide range of m/z ratios, or selected ion monitoring (SIM) mode, to gather data for specifi

....</ref><ref>Fulljames, J. R., L. J. J. Zijerveld, R. C. M. W. Franssen, G. M. Ingram, and P. D. Richard, 1996, Fault seal processes, in Norwegian Petrol ...t has moved past some critical portion of the fault plane.<ref>Skerlec, G. M., 1996, Risking fault seal in the Gulf Coast (abs.): AAPG Annual Convention

...the Paleozoic [[Era]],<ref name=Wengerdandmatheny_1958>Wengerd, S. A., and M. L. Matheny, 1958, [http://archives.datapages.com/data/bulletns/1957-60/dat

...s]] and [[Permeability|permeable]] rocks at shallow depths (less than 3000 m; about 10,000 ft). The geothermal energy is stored in both the solid rock a ...gned to recover heat from impermeable hot dry rocks at depths of 1500–2000 m (5000–6500 ft) by drilling two closely located wells into them, artificia

...asins around the world. In Henry et al.<ref name=Henryetal_2010>Henry, M., M. Pentilla, and D. Hoyer, 2010, [http://archives.datapages.com/data/specpubs ...lsleyandtieman_2010 /><ref name=Wieneretal_2010>Wiener, R. W., M. G. Mann, M. T. Angelich, and J. B. Molyneux, 2010, [http://archives.datapages.com/data

...avity|API]] at 60&deg;F (16&deg;C). Carrigy<ref name=Carrigy_1983>Carrigy, M. A., 1983, [https://www.onepetro.org/journal-paper/SPE-12556-PA Thermal rec

| author = Grant M. Skerlec

| author = Grant M. Skerlec ...anging wall]] and [[footwall]] cutoffs.<ref name=ch10r86>Van Wijhe, D. H., M. Lutz, and J. P. H. Kaasschieter, 1980, The Rotliegend in the Netherlands a

| author = Grant M. Skerlec

...nal disciplines within a subsurface team.<ref name=Shepherd_2009>Shepherd, M., 2009, Oil Field Production Geology: [http://store.aapg.org/detail.aspx?id

| author = J. M. Coleman and D. B. Prior ...s]], and [[evaporite]] [[Sabkha|flats]].<ref name=Coleman_1976>Coleman, J. M., 1976, Deltas: Processes of deposition and models for exploration: Continu

| author = Grant M. Skerlec

...of a nondepleted source. Copyright: Krooss;<ref name=Krooss1987>Krooss, B. M., 1987, Experimental investigation of the diffusion of low-molicular weight ...chanism in shale. However, even in sands for distances greater than 10-100 m, [[Hydrocarbon migration|migration]] by diffusion is insignificant relative

...al tension and the contact angle.<ref name=pt05r152>Teeters, D., Anderson, M. A., Thomas, D. C., 1989, Formation wettability studies that incorporate th ...18/13933-PA</ref> from Shamra and Wunderlich.<ref name=pt05r143>Shamra, M. M., Wundlerlich, R. W., 1985, The alteration of rock properties due to intera

...EPM Core Workshop, n. 2, 416 p.</ref> and Miall.<ref name=pt05r109>Maness, M., and J. G. W. Price, 1977, Well formation characterization by residual hyd ...can be scaled as needed. (Modified from Casey.<ref name=pt05r32>Casey, J. M., 1980, Depositional systems and basin evolution of the Late Paleozoic Taos

| author = Grant M. Skerlec

...such as the giant Fahud and Natih fields.<ref name=Terken_1999>Terken, J. M. J., 1999, The Natih petroleum system of north Oman: GeoArabia, v. 4, no. 2 ..., p. 279–292.</ref> <ref name=Talbotandalavi_1996>Talbot, C. J. and Alavi, M., 1996, The past of a future syntaxis across the Zagros, in G. I. Alsop, D.

...assified into shallow (less than 300m), intermediate (between 300 and 2000 m) and deep drifts (more than 2000m). The most widely used classification (Re * Rebesco M. and A. Camerlenghi, 2008, Contourites: Elsevier Science

...modeling: Definitions and concepts], ''in'' K. E. Peters, D. J. Curry, and M. Kacewicz, eds., [https://archives.datapages.com/data/alt-browse/aapg-speci ...ent will occur between 30-40 °C, for freshwater environment between 20-30 °m³C and for marine environment between 15-20 °C.<ref name="6Das" />

...s.com/data/specpubs/memoir91/CHAPTER11/CHAPTER11.HTM Lithofacies maps], in M. Shepherd, Oil field production geology: [http://store.aapg.org/detail.aspx ...es.com/data/specpubs/memoir91/CHAPTER06/CHAPTER06.HTM Sources of data], in M. Shepherd, Oil field production geology: [http://store.aapg.org/detail.aspx

...(pore throat) radius<ref name=Vavra1992>Vavra, C. L., J. G. Kaldi, and R. M. Sneider, 1992, [http://archives.datapages.com/data/bulletns/1992-93/data/p ...quality of the rock (from Sneider et al.<ref name=Sneider1977>Sneider, R. M., F. H. Richardson, D. D. Paynter, R. E. Eddy, and I. A. Wyant, 1977, Predi

| author = Grant M. Skerlec

...>; Zanella and Coward, 2003<ref name=Zanellaandcoward2003>Zanella, E., and M. P. Coward, 2003, Structural framework, in D. Evans, C. Graham, A. Armour, ...simplified from Fraser et al., 2003<ref name=Fraseretal2003>Fraser, S., A. M. Robinson, H. D. Johnson, J. R. Underbill, D. G. A. Kadolsky, R. Connell, P

Mitchum, R. M., P. R. Vail, and J. B. Sangree, 1977, [http://archives.datapages.com/data/

...called [[pyrobitumen]]. It occurs in veins [[length::1 mm]] to [[length::8 m]] across and appears to have been injected or is a dead seepage.

...experimental setup.<ref name=Panjaetal_2020>Panja, P., Velasco, R., & Deo, M. (2020). Understanding and Modeling of Gas-Condensate Flow in Porous Media. ...uri, F., & Adi P, S. (2015). Analysis Of Condensate Banking Indication Of “M” Gas Condensate Reservoir From Welltesting Examination. Thirty-Ninth Annu

...P., S. J. Clift, D. S. Hamilton, H. S. Hamlin, T. F. Hentz, W. E. Howard, M. S. Akhter, and S. E. Laubach, 1993, Major low-permeability sandstone reser ...'' has been defined as those gas accumulations deeper than 15,000 ft (4572 m);<ref name=Dymanetal_1997>Dyman, T. S., D. D. Rice, and P. A. Westcott, eds

| author = Denise M. Stone

...gnificant surfaces.<ref name=ch17r92>Van Wagoner, J. C., R. M. Mitchum, K. M. Campion, and V. D. Rahmanian., 1990, Siliciclastic sequence stratigraphy i ...rriam-webster.com/dictionary/anoxic anoxic] events<ref name=ch17r5>Arthur, M. A., and W. E. Dean, 1986, Cretaceous paleoceanography, in B. E. Tucholke,

...erence is in the depth to the onset of oil generation, where [[depth::1000 m]] separates the top of the oil windows of these two kerogen types. ! Present-day depth, m, Type II

...5 m (16–50 ft) in height, having a reservoir volume of more than 3 million m³ (177 million ft³). Sites favorable for the building

| author = J. M. Coleman and D. B. Prior ...lain of the Mississippi River delta.<ref name=Colemanetal_1981>Coleman, J. M., and D. B. Prior, 1981, [http://archives.datapages.com/data/specpubs/sands

...11-323.</ref> MacGowan et al.,<ref name=Macgowanetal_1993>MacGowan, D. B., M. Garcia-Gonzales, D. R. Britton, and R. C. Surdam, 1993, Timing of hydrocar ...ky Mountain region are effective for periods of time ranging from 25 to 40 m.y., the lapsed time since formation of most BCGAs in the region. However, a

.../0001/0050/0071.htm Wellbore trajectory], ''in'' D. Morton-Thompson and A. M. Woods, eds., Development geology reference manual: [http://store.aapg.org ...com/data/specpubs/memoir91/CHAPTER28/CHAPTER28.HTM Types of wells], ''in'' M. Shepherd, Oil field production geology, [http://store.aapg.org/detail.aspx

...ref> Deep water is also defined as present-day sea depths in excess of 500 m (1640 ft) deep. ...rock for the province, e.g., the Magnus and Claymore fields.<ref>Shepherd, M., C. J. Kearney, and J. H. Milne, 1990, [http://archives.datapages.com/data

:<math>F = \frac{a}{\phi^{m}}</math> ...e determined from local experience. The most common values for ''a'' and ''m'' are as follows:

...of Economic Geology<ref name=Gherabati>Gherabati, S. A., H. S. Hamlin, K. M. Smye, R. L. Eastwood, F. R. Male, and G. McDaid, 2019, Evaluating hydrocar General Structure Map (Pollastro et al.<ref name=Pollastroetal>Pollastro, R. M., L. N. R. Roberts, and T.A. Cook, 2012, Geologic model for the assessment

...[[nose]] and [[closure]]. The oil column is [[length::70 ft]] [[depth::(20 m]]) and exceeds structural closure. This is a combination [[Structural trap

...urrence: New York, Springer-Verlag, 538 p.</ref><ref name=pt05r81>Hunt, J. M., 1979, Petroleum Geochemistry and Geology: San Francisco, CA, W. H. Freema ...from molecular composition data.<ref name=pt05r94>Kennicutt, M. C., and J. M. Brooks, 1988, Surface geochemical exploration studies predict API gravity

...j.jappgeo.2020.104054</ref> Hange et al.<ref name=Hangeetal_2019>Hanga, K. M., & Kovalchuk, Y. (2019). Machine learning and multi-agent systems in oil a ...ortant variable for the production engineers.<ref name=Miahetal_2020>Miah, M. I., Zendehboudi, S., & Ahmed, S. (2020). Log data-driven model and feature

...fied from Hermanrud et al. (2014<ref name=Hermanrudetal2014>Hermanrud, C., M. E. Hakjelsvik, K. Kristiansen, A. Bernal, and A. C. Strömbäck, 2014, Col ...aphy of the greater Barents Sea: Implications for petroleum systems, in A. M. Spencer, A. F. Embry, D. L. Gautier, A. V. Stoupakova, and K. Sørensen, e

...rs.<ref name=Richardsonetal_1988a>Richardson, J. G., J. B. Sangree, and R. M. Sneider, 1988, Eolian dunes: Journal of Petroleum Technology, v. 40, no. 1 ...ne in northern Arizona. The average thickness of cross-bed sets is about 6 m (20 ft). The width-to-thickness ratio is estimated as between 50:1 and 100:

| author = Grant M. Skerlec ...ety of Petroleum Engineers, paper 12967.</ref><ref name=ch10r96>Yaxley, L. M., 1987, Effect of a partially communicating fault on transient pressure beh

...>Cheatham, C., 1992, [[Wellbore trajectory]], in D. Morton-Thompson and A. M. Woods, eds., Development geology reference manual: [http://store.aapg.org/ At very high angles, if the top reservoir is 15 m (49 ft) deeper than predicted, the target will be penetrated much later tha

| author = John M. Armentrout ...gh Island–East Breaks depocenter, has more than [[depth::16,000 ft]] (4875 m) of late Pliocene and early Pleistocene sediments deposited during a succes

| author = John M. Armentrout ...C5-11D7-8645000102C1865D.</ref><ref name=ch04r117>Winker, C., D., Edwards, M., B., 1983, Unstable progradational clastic shelf margins: SEPM Special Pub

...k. After Ringrose and Corbett.<ref name=ch07r11>Ringrose, S. P., and P. W. M. Corbett, 1994, Controls in two phase fluid flow in heterogeneous sandstone

* Fatahillah, M. R., 2011, Efek Teknik Hydraulic Fracturing dalam Eksplorasi Shale Gas di A

| author = John M. Armentrout

...deling: Overview with examples from the Bahamas], ''in'' G. M. Grammer, P. M. Harris, and G. P. Eberlie, eds., Integration of outcrop and modern analogs ...dern day carbonate environments.<ref name=Harrisandkowalik_1994>Harris, P. M., and W. S. Kowalik, eds., 1994, Satellite images of carbonate depositional

| author = John M. Armentrout

...tries as either sheets or ribbons.<ref name=Friendetal_1979>Friend, P. F., M. J. Slater, and R. C. Williams, 1979, [http://jgs.geoscienceworld.org/conte ...Permian, Baylor County, Texas (from Burnett<ref name=Burnett_1996>Burnett, M., 1996, [http://archives.datapages.com/data/specpubs/study42/ch05/0062.htm

...“biosteering” in hydrocarbon reservoir exploitation. In Koutsoukos, E. A. M. (ed.). Applied Stratigraphy, 339 – 355. Springer.</ref> See also Holmes, ...P. R. 1994. Biostratigraphic steering of horizontal wells. In Al-Husseini, M. I. (ed.). The Middle East Petroleum Geosciences. Selected Middle East Pape

...rocarbon-induced alteration of soils and sediments], in Schumacher, D.,and M. A. Abrams, eds., Hydrocarbon Migration and Its Near-Surface Expression: [h

Meyer et al.<ref name=ch18r27>Meyer, W., T., Lovell, J., S., Hale, M., 1983, Detection of concealed mineral and energy resources by vapor geoche

...quina, ''in''' H. A. Leanza, C. Arregui, O. Carbone, J. C. Daniela, and J. M. Vallés, eds., Geología y Recursos Naturales de la Provincia del Neuquén ...pionellid biozones.<ref>Kietzmann, D. A., R. M. Palma, A. C. Riccardi, J. M. Chivelet, and J. López-Gómez, 2014, Sedimentology and sequence stratigra

The E-field is measured with a grounded dipole typically 50–200 m long. All subsurface geology information is contained in the E-field data.

| author = M. L. Bordenave ...hore (after Bordenave and Hegre<ref name=Bordenaveandhegre_2005>Bordenave, M. L. and Hegre, J. A., 2005, [http://onlinelibrary.wiley.com/doi/10.1111/j.1

...11-323.</ref> MacGowan et al.,<ref name=Macgowanetal_1993>MacGowan, D. B., M. Garcia-Gonzales, D. R. Britton, and R. C. Surdam, 1993, Timing of hydrocar ...e 3]]). Individual reservoirs range in thickness from 15 to 125 ft (4.6-38 m). Gas reservoirs are saturated and contain water at irreducible levels. The

...; Banerjee et al., 2002<ref name=Banerjeeetal2002>Banerjee, A., S. Pahari, M. Jha, A. K. Sinha, A. K. Jain, N. Kumar, et al., 2002, The effective source ...hetal2005>Singh, A. K., J. R. Sethi, A. K. Rai, S. Kumar, J. Kundu, and S. M. Goel, 2005, An overview of exploration and exploitation strategy for hydro

| author = Grant M. Skerlec

| author = Roger M. Slatt, William E. Galloway ...Cretaceous), Kuparuk field, North Slope, Alaska, in A. J. Lomando, and P. M. Harris, eds., Giant oil and gas fields—A core workshop: Society of Econo

...and pressures, it undergoes a process called separation migration. At 2500 m, the 100 tons of single phase have separated into 40 tons of gas and 60 ton

...oil from the center of the pores (from Clark et al).<ref>Clark, N. J., H. M. Shearin, W. P. Scultz, K. Garms, and J. L. Moore, 1958, Miscible drive—I ...s termed the wettability.<ref name=Vavra>Vavra, C. L., J. G. Kaldi, and R. M. Sneider, 1992, [http://archives.datapages.com/data/bulletns/1992-93/data/p

...rk Thomas 2006" /><ref name="Watson and Harrison 2005">Watson, E. B., & T. M. Harrison, 2005, Zircon Thermometer Reveals Minimum Melting Conditions on E ...b|Optical microscope photograph; the length of the crystal is about 250 [[µm]].]]

[[File:Aapg 8.png|400px|thumbnail|center|Figure 8 Kind of DHI.<ref>Bacon, M., R. Simm, and T. Redshaw, 2003, 3D Seismic Interpretation. Cambridge Unive ...ow The Anomaly of Strong Amplitude that Indicating of Reservoir<ref>Taner, M. T and R. E. Sheriff, R.E. [http://archives.datapages.com/data/specpubs/sei

| author = John M. Armentrout

...r, O = outer, I = inner. (From Armentrout.<ref name=pt05r20>Armentrout, J. M., 1987, Integration of biostratigraphy and seismic stratigraphy, Pliocene-P ...series]], and [[stratigraphic stage|stages]].<ref name=pt05r72>Hancock, J. M., 1977, The historic development of biostratigraphic correlation, in E. G.

| author = John M. Armentrout

...sinar3/data/a134/a134/0001/0650/0681.htm The Paraná Basin, Brazil], ''in'' M. W. Leighton, D. R. Kolata, D. F. Oltz, and J. J. Eidel, eds,. Interior cra .... E. Jordan, R. W. Allmendinger, C. Mpodozis, J. M. Kay, J. M. Cortés, and M. Palma, 1986, Paleozoic terranes of the central Argentine-Chilean Andes: Te

...sent-day location of hydrocarbon fields.‎<ref name=Neumaier_2016>Neumaier, M., 2016, Structural restoration and basin and petroleum systems modeling: Ca ...e deformation in a.‎<ref name=Morettietal_2006>Moretti, I., F. Lepage, and M. Guiton, 2006, KINE3D: A new 3D restoration method based on a mixed approac

| author = Grant M. Skerlec

...cephalic] area and may have functioned as teeth.<ref name=ch17r71>Purnell, M. A., 1995, Microwear on conodont elements and macrophagy in the first verte

...rease until 53.9% with average 36.6%. Kabs data before vibration is 231.46 m – 1113.59 mD and after vibration can reach 54.1% with average 39.4%. Sor * Cs=wave velocity shear (m/sec)³ .

:<math>\text{F} = \frac{a}{\mathit{\Phi}^m}</math> ...he porosity, and Sw is the water saturation. To acquire the value of a and m, the user will need to create a pickett plot, but according to Asquith,<ref

...., V. F. Nuccio, T. S. Dyman, T. A. Gognat, R. C. Johnson, J. W. Schmoker, M. S. Wilson, and C. Bartberger, 2001, Basin-centered gas systems of the U.S. ...igh || Tertiary || Direct || Law et al.,<ref name=Lawetal_1994>Law, B. E., M. E. Tennyson, and S. Y. Johnson 1994, Basin-centered gas accumulations in t

...seful for mapping paleogeomorphology and faults.<ref name=ch21r4>Bahorich, M., S., Farmer, S., L., 1995, 3-D seismic discontinuity for faults and strati

...m Engineers Paper No. 13226, 15 p.</ref><ref name=Smith el al._1985>Smith, M. B., N.-K. Ren, G. G. Sorrells, and L. W. Teufel, 1985, A comprehensive fra ...for orientation. Studies by Hocker et al.<ref name=pt03r23>Hocker, C., K. M. Eastwood, J. G. Herweijer, and J. T. Adams, 1990, [http://archives.datapag

...the well. Drafted from data in Hoversten.<ref name=Hoversten>Hoversten, G. M., 1996, Papua New Guinea MT: looking where seismic is blind: Geophysical Pr

| author = J. H. Justice, M. E. Mathisen, J. R. Bulau, A. A. Vassiliou ..., Reservoir Geophysics, p. 321–334.</ref><ref name=pt07r27>Justice, J. H., M. E. Mathisen, A. A. Vassiliou, I. Shiao, B. R. Alameddine, and N. J. Guinzy

...ctor once the correct semilog straight line is identified and its slope, ''m'', is estimated. These equations apply to both drawdown and buildup tests. :<math>s = 1.151 \left[\frac{\Delta p_{1{\rm hr}}}{m} - \log \left(\frac{k}{\phi \mu c_{\rm t}r_{\rm w}^{2}}\right) + 3.23\right

...hronostratigraphic chart shows the following:<ref name=ch21r31>Mitchum, R. M., P. R. Vail, J. B. Sangree, 1977, [http://archives.datapages.com/data/spec

...an often be used to guide the modeling process.<ref name=pt10r29>Slatt, R. M., Hopkins, G. L., 1990, Scaling geologic reservoir description to engineeri ...y profile in noncored wells is of prime importance.<ref name=pt10r38>Wolf, M., Pelissier-Combescure, J., 1982, Faciolog-automatic electrofacies determin

...e been proposed (Villegas et al., 1994<ref name=Villegasetal1994>Villegas, M., S. Bachu, J. C. Ramon, and J. Underschultz, 1994, Flow of formation water ..., no. 4, p. 569–586.</ref>, 2010<ref name=Goncalvesetal2010>Gonçalvès, J., M. Pagel, S. Violette, F. Guillocheau, and C. Robin, 2010, Fluid inclusions a

...filling and emptying of the Ula oilfield (Norwegian North Sea), ''in'' J. M. Cubitt and W. A. England, eds., The geochemistry of reservoirs: Geological ...of 10-2 ms-1 for a fluid of 1 cp (centipoise) under a pressure of 10-4atm m-2. Permeability in reservoir rocks may range from 0.1 mD to more than 10 D.

| author = Grant M. Skerlec

.../ref> Exxon workers<ref name=ch21r47>Van Wagoner, J. C., R. M. Mitchum, K. M. Campion, and V. D. Rahmanian, 1990, Siliciclastic Sequence Stratigraphy in

...9.</ref><ref name=Tuttleetal_1999>Tuttle, M. L. W., R. R. Charpentier, and M. E. Brownfield, 1999, [http://greenwood.cr.usgs.gov/energy/WorldEnergy/OF99 ...t, 1975, Modern river deltas: Variability of processes and sand bodies, in M. L. Broussard, ed., Deltas, models for exploration: Houston Geological Soci

...tities being measured on each. Suppose that the n samples are divided into m classes or groups. Discriminant analysis consists of two steps: ...makes each group different from the others. The answer may be that not all m predefined groups are significantly different from each other.

| author = John M. Armentrout

| author = John M. Armentrout

* h = thickness of the hydrocarbon column, ft or m

.../0001/0000/0031.htm Structural and stratigraphic uses of dip profiles], in M. T Halbouty, ed., Deliberate Search for the Subtle Trap: [http://store.aapg ...escribed or by cubic spline interpolation.<ref name=McCoss_1987>McCoss, A. M., 1987, [http://www.sciencedirect.com/science/article/pii/0191814187900599

...rdepositional systems. After Mitchum, et al.<ref name=ch21r31>Mitchum, R., M., Vail, P., R., Sangree, J., B., 1977, [http://archives.datapages.com/data/

...analysis. From Seifert et al.<ref name=Seifertetal_1980>Seifert, W. K., J. M. Moldowan, and R. W. Jones, 1980, Application of biological marker chemistr ...2 | Map ID || rowspan = 2 | [[Accumulation]] || rowspan = 2 | Res. depth (m) || rowspan = 2 | Trap type || colspan = 2 | In Place || colspan = 2 | Cum

| author = Bradley M. Robinson ...ning'' can occur when the oil is produced. Muskat<ref name=pt09r18>Muskat, M., 1949, Physical principles of oil production: New York, McGraw-Hill, chap.

...er than changes in natural hydrodynamic regimes.<ref name=ch11r15>Hubbert, M. K., 1953, [http://archives.datapages.com/data/bulletns/1953-56/data/pg/003

:<math>h = \frac{P}{(\rho_{\rm w} \times C)} + (E_{\rm m} - E_{\rm r})</math> * ''C'' = pressure gradient constant (0.433 psi/ft or 0.1 kg/cm²/m)

| author = W.J. Ebanks, M. H. Scheihing, C. D. Atkinson ...lithological, well test, and production data<ref name=pt06r129>Sneider, R. M., F. H. Richardson, D. D. Paynter, R. R. Eddy, and I. A. Wyant, 1977, [http

...d following multiple fracture treatments in an interval about 2400 ft (732 m) thick (R. E. Mueller, 2002, personal communication). ...ell, approximately 76 natural fractures were recorded from a 78.2 ft (23.8 m)-long core taken from the same horizontal leg.<ref name=Lorenzandmroz_1999>

...name=Johnsonetal_1999>Johnson, R. C., R. A. Crovelli, B. G. Lowell, and T. M. Finn, 1999, [http://pubs.er.usgs.gov/publication/ofr99315A An assessment o ...., V. F. Nuccio, T. S. Dyman, T. A. Gognat, R. C. Johnson, J. W. Schmoker, M. S. Wilson, and C. Bartberger, 2001, Basin-centered gas systems of the U.S.

...plot is made on Cartesian coordinate paper. A straight line with slope, ''m''′, should result; this slope is used in Equation 4 to calculate permeabi :<math>k = \frac{1637T\mu z}{m'h}</math>

Correlation between matrix porosity (φ_m) and fracture porosity (φ_f), is matrix porosity that refe ...d total of matrix in rock is scaled in bottom. With matrix porosity (φ_m), water saturated part, oil saturated part, and each parts are expres

...vely fresh and oil mud systems || rowspan=3 | Not recommended; Res > 200 Ω-m or ''R''_mf / ''R''_w < 2.5 ...tems; reduced shoulder effects || rowspan=3 | Not recommended; Res > 250 Ω-m or R_mf / ''R''_w < 2.5

| author = Grant M. Skerlec

...name=ch17r75>Ruddiman, W. F., Raymo, M. E., Martinson, D. G., Clement, B. M., Backman, J., 1989, Pleistocene evolution: Northern Hemisphere ice sheets ...numerical age. The accuracy of the resulting age estimates approaches ±1.0 m.y for the [[Cenozoic]] intervals.

...ard interpretation; part 4—wireline methods], in D. Morton-Thompson and A. M. Woods, eds., Development Geology Reference Manual: [http://store.aapg.org/

* Ahr, W. M., 2008, Geology of Carbonate Reservoirs: United States: John Wiley & Sons, ...nd their application to sedimentologic and paleoenvironmental problems, in M. A. Arthur (Ed.), Stable Isotopes in Sedimentary Geology: SEPM Short Course

...nipe_1992>Knipe, R. J., 1992, Faulting processes and fault seal, ''in'' R. M. Larsen, H. Brekke, B. T. Larsen, and E. Talleraas, eds., Structural and te * H = hydrocarbon column height (m /ft, where 1 m = 3,2808 ft)

* Amyx, J., M. D. Bass, and L. R. Whiting, 1960, Petroleum Reservoir Engineering: New Yor * Bass, D. M., Jr., 1987, Properties of reservoir rocks, ''in'' H. Bradley, ed., Petrole

| author = Grant M. Skerlec ...do, demonstrate that 57 bcf of gas can diffuse from a trap in only 0.5–5.0 m.y.<ref name=ch10r59 />

...arshore aquatic environments. From Robinson;<ref name=ch08r46>Robinson, K. M., 1987, An overview of [[source rock]]s and oils in Indonesia: Proceedings, ...AAPG Memoir 51], p. 403–423.</ref><ref name=ch08r17>Guthrie, J. M., and L. M. Pratt, 1995, [http://archives.datapages.com/data/bulletns/1994-96/data/pg/

...bon-induced alteration of soils and sediments], in Schumacher, D., Abrams, M., A., eds., Hydrocarbon Migration and Its Near-Surface Expression: [http://

...et al.<ref name=pt07r49>Reynolds, R. L., M. Webring, V. J. S. Grauch, and M. Tuttle, 1990, Magnetic forward models of Cement oil field, Oklahoma, based

Large clinoform geometries (100s to 1000s m) are a classic feature in many super basins, like in Neuquén, West Siberia ...ribution of source rocks.<ref name=Vailandmitchum_1979>Vail, P. R., and R. M. Mitchum, 1979, [https://archives.datapages.com/data/specpubs/history2/data

...borne instruments generally limited in penetration to 100 to [[length::200 m]]. Airborne electromagnetic surveys have proven very effective for mapping ...ited from less than [[length::0.3 m]] in silty soils to over [[length::100 m]] in permafrost, freshwater-saturated sand, and some very low porosity rock

[[file:difficult-lithologies_fig1.png|thumb|300px|{{figure number|1}}M-N crossplot for mineral identification. &copy; Schlumberger Well Services, ...ques are commonly used to identify the occurrence of mineralogies: (1) the M-N crossplot and (2) the MID crossplot.

...formation into the well bore ([[:Image:Charles-l-vavra-john-g-kaldi-robert-m-sneider_capillary-pressure_1.jpg|Figure 1b]]). A screen and liner completio ...terval is produced at a time ([[:Image:Charles-l-vavra-john-g-kaldi-robert-m-sneider_capillary-pressure_3.jpg|Figure 3b]]). A single completion is simpl

...of Business Administration, 402 p.</ref> and Walls<ref name=pt02r19>Walls, M. R., 1989, Assessing the corporate utility function—a model for the oil a

...ate cementation in petroleum reservoirs, in Schneidermann, N., Harris, P., M., eds., Carbonate Cements: SEPM Special Publication 36, p. 97–106.</ref>

Corbett, K., Friedman, M., Spang, J., 1987, Fracture Development and Mechanical Stratigraphy of Aust Gent, H., Holland, M., Urai, J., Loosveld, R., 2009, Evolution of Fault Zones in Carbonates with

| author = Denise M. Stone

| author = Grant M. Skerlec

...ks in Pinedale field occur at depths of about 8500 to 14,500 ft (2600–4400 m) and are tight with fairly low porosity (mostly <10%) and very low (micro-D ...ntration of gas is in part due to the tremendous thickness (∼6000 ft, 1800 m) of the gas-saturated Lance and upper Mesaverde sections that comprise the

| author = John G. Kaldi, Catherine M. Gibson-Poole, Tobias H. D. Payenberg ...to selection and evaluation of CO₂ geosequestration sites], in M. Grobe, J. C. Pashin, and R. L. Dodge, eds., Carbon dioxide sequestration i

| author = J. M. Coleman and D. B. Prior ...posits display high lateral continuity but are rather thin (rarely over 30 m thick).

:where σ is the unit weight of the overlaying rock [mN/ m³]. :z is the depth to point below surface [m].

| author = S. P. Grier, D. M. Marschall ...later degradation by compaction or cementation.<ref name=pt06r158>Wilson, M. D., Pittman, E. D., 1977, Authigenic clays in sandstones—recognition and

...differ from those of adjacent facies units”.<ref name=ch21r31>Mitchum, R., M., Vail, P., R., Sangree, J., B., 1977, [http://archives.datapages.com/data/

| author = Jeremy M. Boak ...Slatt et al.<ref name=pt06r122>Slatt, R. M., S. Phillips, J. M. Boak, and M. B. Lagoe, 1993, Scales of geological heterogeneity of a deep-water sand gi

...petroleum inclusions were found in gas-stage TSR calcite, well D4, 4793.00 m (15,721.04 ft).<ref name=Jiangetal_2014>Jiang, Lei, Richard H. Worden, and ...ef> Thin sections must be carefully ground to final thickness (usually 30 μm) to avoid fracturing and plucking.

| author = Denise M. Stone

* Kelly height or [[rate of penetration]] (ROP) (in ft/hr, m/hr, or min/ft) * Depth (in ft or m)

...v. 19, no. 6, p. 617-620.</ref><ref name=Hardyandford_1997>Hardy, S., and M. Ford, 1997, [http://onlinelibrary.wiley.com/doi/10.1029/97TC01171/full Num ...l compaction of interbedded sandstone and coal], ‘’in’’ J. W. Cosgrove and M. S. Ameen, eds., Forced folds and fractures: Geological Society of London S

...d Hammes, 2010). Reservoir depth ranges from 9,000 to 14,000 ft (3000–4700 m), and lateral drilling distances range between 4,600-10,000’ using slick

...l is 100 ft. (From Braithwaite et al.)<ref name=pt06r16>Braithwaite, C. I. M., Marshall, J. D., Holland, T. C., 1989, [https://www.onepetro.org/conferen ...5.htm Strachan and Ricinus West gas fields], Alberta, Canada, in Halbouty, M. T., ed., Giant Oil and Gas Fields of the Decade 1968–1978: AAPG Memoir 3

...at magmatic bodies of small size (2–4 km in diameter and approximately 500 m thick) of laminar geometries and disposal consistent with available subhori ...]] of the fold. Taken from Hansen & Cartwright.<ref>Cartwright, J., and D. M. Hansen, 2006, The three-dimensional geometry and growth of forced folds ab

...dered dense if the line spacing is less than about 1/4 mile [1,320 ft; 400 m].) The advantages of 3-D include the following:

...the impact of compressing seismic sections on a workstation. A 6.4-km, 32-m-deep valley network incised in the Muddy Formation (Lower Cretaceous) is di

...is also equal to the gas molecular weight divided by air molecular weight (M_air = 28.97). Denoted mathematically as γ_g (where air | M₇₊

...From Meyer and Nederlof.<ref name=Meyerandnederlof_1984>Meyer, B. L., and M. H. Nederlof, 1984, [http://archives.datapages.com/data/bulletns/1984-85/da

...ood example is found in Seifert et al.<ref name=ch08r49>Seifert, W. K., J. M. Moldowan, and R. W. Jones, 1979, Application of biological marker chemistr

...03r21>Flopetrol-Johnston, 1987, Downhole testing services brochure, p. DTS/M-28[5-87].</ref>.)]] | ''m''

...tion Volume Investigated, ft³ || Formation Volume Investigated, m³

...s of fractured reservoir types 1 through 3 and normal matrix reservoirs (''m'') in the percentage of porosity and permeability space. Symbols: ''k''<sub ...l models of fracture system genesis.<ref name=pt06r135>Stearns, D. W., and M. Friedman, 1972, [http://archives.datapages.com/data/specpubs/fieldst4/data

| author = Denise M. Stone

...100 ft]] (30 m) near the crest of the structure to [[length::500 ft]] (150 m) on the flanks. The dashed contours are the oil/water and gas/oil contacts.

Numbered peaks are hopanes. T_s and T_m are, respectively, 18α(H)-22,29,30-trisnorneo-hopane and 17α(H)-22,

| author = Gerard C. Gaynor, Robert M. Sneider ...y,<ref name=pt06r53 /> and Sneider and King.<ref name=pt06r128>Sneider, R. M., and H. R. King, 1984, [http://archives.datapages.com/data/specpubs/fields

...e saline lake basin<ref name=Kng2012>Kuang, L., Y. Tang, D. Lei, Q. Chang, M. Ouyang, L. Hou, and D. Liu, 2012, Formation conditions and exploration pot

...logging: the mudlog|Mudlogging: The mudlog]], in D. Morton-Thompson and A. M. Woods, eds., [http://archives.datapages.com/data/alt-browse/aapg-special-v ...asurements (Monicard, 1980). Vertical core plugs may also be cut every 1.5 m (5 ft) for example. On occasions, large pieces of full-diameter core are us

| author = Grant M. Skerlec

...0.5 and 2 km (0.3 and 1.2 mi) wide.<ref>Major, R. P., D. G. Bebout, and P. M. Harris, 1996, Facies heterogeneity in a modern ooid sand shoal—An analog ...: Outcrop model for Cretaceous carbonate reservoirs], in G. M. Grammer, P. M. Harris, and G. P. Eberli, eds., Integration of outcrop and modern analogs

...182-PA</ref> and Wilson and Hensel<ref name=pt05r170>Wilson, D. A., and W. M. Hensel, Jr., 1978, Computer log analysis plus core analysis equals improve ...ctions of the Sixth European Formation Evaluation Symposium, London, Paper M.</ref> have used multiple regression, together with log and core data, to p

...: Los Angeles, Trija Publishing Co., 1195 p.</ref><ref name=ch14r1>Dobrin, M. B., 1960, Introduction to Geophysical Prospecting, 2nd ed.: New York, McGr

| author = P. J. Hicks Jr., C. M. Fraticelli, J. D. Shosa, M. J. Hardy, and M. B. Townsley ...pe paths are shown in green. The scale bar in the legend represents 12,500 m (41,010 ft).

..., 1971, Lower Ordovician conodonts in North America, in W. C. Sweet and S. M. Bergstrom, eds., Symposium on conodont biostratigraphy: Geological Society ...al.<ref name=Ferrusquiavillafrancaetal_2009>Ferrusquia-Villafranca, I., R. M. Easton, and D. E. Owen, 2009, Do GSSPs render dual time-rock/time classifi

...gging allows selective sampling of specific zones.<ref name=pt05r38>Craft, M., and D. K. Keelan, 1985, Coring, Part 7—analytical aspects of sidewall c ...g processes, gas expansion, and handling errors.<ref name=pt05r22>Bass, D. M., 1987, Properties of reservoir rocks, in Bradley, H. B., ed., Petroleum En

...Association of Drilling Contractors (IADC).<ref name=pt08r18>Rose, R. J., M. R. Taylor, and R. E. Jantzen, 1989, Information transfer standards for wel

...sent a worse-case scenario. Permeability of the formation rock to a 0.51-''M'' (3 wt. %) NaCl solution is followed by permeability to freshwater. Sensit ...te clays, respectively.<ref name=pt05r139>Scheuerman, R. F., Bergersen, B. M., 1990, Injection-water salinity, formation pretreatment, and well operatio

| author = Grant M. Skerlec

...w to operate an RFT survey (see Gunter & Moore<ref name=ch05r9>Gunter, J., M., Moore, C., V., 1987, Improved use of wireline testers for reservoir evalu

Sneider and King<ref name=ch09r57>Sneider, R., M., King, H., R., 1984, [http://archives.datapages.com/data/specpubs/fieldst4

...h's gravity field is typically about 980 Gal.<ref name=pt07r58>Telford, W. M., Geldart, L. P., Sheriff, R. E., Keys, D. A., 1976, Applied Geophysics: Ca

Erenpreiss, M.S., Wickstrom, L.H., Perry, C.J., Riley, R.A., Martin, D.R., and others, 20 ...C., Trippi, M., Le, P., Brownfield, M., Woodall, C., Marra, K., Tennyson, M., 2019. Assessment of undiscovered gas resources in the Middle Devonian Mar

| author = J. M. Coleman and D. B. Prior ...iving [[fluvial]] sediment. This area ranges in water depth from 50 to 300 m and in width from a few kilometers to tens of kilometers. It is the foundat

...crystalline), dolomicrite / micrite dolomite / microlite (crystal size <1 µm), dolosparite, dololutite (clay or mud size, <1/16 mm), dolosiltite (silt s ...identification (Fig. 16; Rider, 1996; Zangana et al., 2020). In addition, M-N cross-plot is also usually used to determine lithology of geological form

* Karamouz,M., A. Ahmadi, and M. Akhbari, 2012, Groundwater hydrology: Engineering, planning, and managemen

...matter. See Duddy et al<ref name=ch06r4>Duddy, I. R., P. F. Green, and G. M. Laslett, 1988, Thermal annealing of fission tracks in apatite—3, variabl

: <math>\mu_o = \mu_{ob} \left ( \frac{P}{P_b} \right )^m</math> : <math>m = 2.6P^{1.187} \exp [-11.513 - 8.98 \times 10^{-5} \times P]</math>

| author = O. R. Lazar, K. M. Bohacs, J. Schieber, J. H. S. Macquaker, T. M. Demko ...aapg-sp2160035.htm Tools and techniques for studying mudstones], ‘’in’’ K. M. Bohacs and O. R. Lazar, eds., Sequence stratigraphy: Applications to fine-

...e-house worlds, in J. F. Read, C. Kerans, L. J. Webber, J. F. Sarg, and F. M. Wright, eds., Milankovitch Sea-level Changes, Cycles, and Reservoirs on Ca

...ophic discharge. And incised-channel flow takes place through channel, 1-4 m high, incised into the upper fan. ...aas which is gigantic bedform that has up to 5,5 km long and height of 400 m (Wilson, 1972; McKee, 1982). Environments of deserts are divided into 3 mai

...disappears after 5-15 million years , while the effect from sills up to 20 m thick disappear after 15,000 years (Figure 10). ...the rock blocks (V.S. Staroseltsev, V.M. Lebedev, F.Yu. Levinson-Lessing, M.G. Ravich, L.A. Chaika, P.E. Offman, etc.). Another school, on the contrary

...in amplitude.<ref name=Dalleyetal_1989>Dalley, R. M., E. E. A. Gevers, G. M. Stampli, D. J. Davies, C. N. Gastaldi, P. R. Ruijetnberg, and G. J. D. Ver ...eakly, D. C., 1992, [[Core orientation]], ''in'' D. Morton-Thompson and A. M. Woods, eds., Development geology reference manual: [http://store.aapg.org/

...s (10–500 k.y) and, to a lesser extent, long-term third-order cycles (1–10 m.y). Early diagenesis that takes place during fourth- or fifth-order cycles ...ds, in Read, J., F., Kerans, C., Webber, L., J., Sarg, J., F., Wright, F., M., eds., Milankovitch Sea-level Changes, Cycles, and Reservoirs on Carbonate

| author = Arnold M. Woods, Byram Reed

...esses of sedimentary rocks are about 2000 m in the Chad basin and only 500 m in the Sokoto embayment. * Vérard, C., C. Hochard, P. O. Baumgartner, and G. M. Stampfli, 2015, Geodynamic evolution of the Earth over the Phanerozoic: Pl

Şengör, A. M. C. and Y. Yilmaz, 1981, Tethyan evolution of Turkey, A plate tectonic appr ...<ref name=Sengoretal_2005>Şengör, A. M. C., Tüysüz, O., İmren, C., Sakinç, M., Eyidoǧan, H., Görür, N., Le Pichon, X., and Rangin, C., 2005, The Nort

...rough Miocene rocks. Clayton and Koncz<ref name=ch08r6>Clayton, C. J., and M. Bjorøy, 1994, Effect of maturity on 13C/12C ratios of individual compound

...ges from 25,000 to 100,000 mg/1 per [[depth::1000 ft]] (80 to 300 mg/1 per m).<ref name=ch05r6>Dickey, P. A., 1969, Increasing concentration of subsurfa

* Sercombe, W. J., B. R. Golob, M. Kamel, J. W. Stewart, G. W. Smith, and J. D. Morse, 1997, Significant stru ...stratigraphic uses of dip profiles in petroleum exploration], in Halbouty, M., T., ed., The Deliberate Search for the Subtle Trap: [http://store.aapg.or

...evolution of the Lower Cretaceous Dakota Group, Western Interior, USA, in M. V. Caputo, J. A. Peterson, and K. J. Franczyk, eds., Mesozoic Systems of t

| author = John M. Armentrout

...tylolitization. A [[cross section]] from Longman<ref name=pt06r78>Longman, M. W., T. G. Fertal, and J. S. Glennie, 1983, [http://archives.datapages.com/ ...aceous), Kuparuk field, North Slope, Alaska, in Lomando, A. J., Harris, P. M., eds., Giant oil and gas fields—A core workshop: Society of Economic Pal

...da, Reprint Series 1, p. 297–319.</ref> and Rider<ref name=pt06r110>Rider, M. H., 1986, Geological interpretation of well logs: New York, John Wiley, 17 ...lting sandstone bodies (e.g., Sneider et al.<ref name=pt06r130>Sneider, R. M., C. N. Tinker, and L. D. Meckel, 1978, Deltaic environment reservoir types

...ts is the zonation of Tipsword et al.<ref name=ch17r85>Tipsword, H. L., F. M. Setzer, and F. L. Smith, Jr., 1966, Interpretation of depositional environ

| author = Arnold M. Woods

...cept sensu Stampfli and Borel.<ref name=Stampfliandborel_2002>Stampfli, G. M., and Borel, G. D., 2002, A plate tectonic model for the Paleozoic and Meso ...li,<ref name=Vonraumerandstampfli_2008>von Raumer, J. F., and Stampfli, G. M., 2008, The birth of the Rheic Ocean - Early Palaeozoic subsidence patterns

...had an oil [[accumulation]] in the vicinity.<ref name=pt05r175>Zarella, W. M. 1967, Analysis and significance of hydrocarbons in subsurface brines: Geoc

Dong, T., He, S., Chen, M., Hou, Y., Guo, X., Wei, C., Han, Y., Yang, R., 2019. Quartz types and orig

...Petroleum Engineers.</ref> and Craft et al.<ref name=pt10r7>Craft, B. C., M. Hawkins, and R. E. Terry, 1991, Applied Petroleum Reservoir Engineering, 2

...onecipher et al.<ref name=ch09r60>Stonecipher, S. A., R. D. Winn, Jr., and M. G. Bishop, 1984, [http://archives.datapages.com/data/specpubs/sandsto2/dat

| author = M. Peter Cone, David G. Kersey ...between detrital grains. Microporosity exists as small pores (less than 2 μm) commonly associated with detrital and authigenic clay minerals. Dissolutio

...nt a worse-case scenario. [[Permeability]] of the formation rock to a 0.51-M (3 wt. %) NaCl solution is followed by permeability to freshwater. Sensitiv ...n extraction can result in dispersible particles.<ref name=Reed_1977>Reed, M. G., 1977, Formation [[permeability]] damage by mica alteration and carbona

| author = Peter M. Duncan ...ver offset is zero at the center of the gather and increases to about 2000 m deep on either end. The offset related curvature of the reflections is due

...ostracods<ref name=ch17r1>Ainsworth, N., R., Burnett, R., D., Kontrovitz, M., 1990, Ostracod colour change by thermal alteration, offshore Ireland and

...an estimated 8% of global oil reserves.<ref name=Bordenave_2014>Bordenave, M. L., 2014, [http://archives.datapages.com/data/specpubs/memoir106/data/505_

...Modified from Coleman and Roberts;<ref name=ColemanRoberts1991>Coleman, J. M., and H. H. Roberts, 1991, Mississippi River depositional system: model for

...n the south and west sides<ref name=ch11r19>Kodl, E. J., J. C. Eacmen, and M. G. Coburn, 1990, A geologic update of the emplacement mechanism within the

...et al.<ref name=Dvgl2011>Deveugle, P. E. K., M. D. Jackson, G. J. Hampson, M. E. Farrell, A. R. Sprague, J. Stewart, and C. S. Calvert, 2011, [http://ar ...on, Special Publication 309, p. 99–121.</ref><ref name=Jckson2009>Jackson, M. D., G. J. Hampson, and R. P. Sech, 2009, [http://archives.datapages.com/da

| author = Daniel M. Jarvie ...); and calcite, in [[metagenesis]].<ref name=J&J2007>Jarvie, B. M., and D. M. Jarvie, 2007, [http://wwgeochem.com/references/JarvieandJarvie2007ThermalD

* Cavalcanti, T. V. D., V., K. Mohaddes, and M. Raissi, 2012, Commodity Price Volatility and the Sources of Growth: IMF Wo

Assume the Oily Co., lessee, obtains oil and gas leases from I. M. Lucky, lessor, who owns a 3/4 interest in a [[area::20 acre]] tract of lan | I. M. Lucky, lessor, 20-ac tract || 0 || 6.25^a x 3/4 x 1/8 || = 00.58

...reas the coefficient itself is the main focus in AVO analysis <ref>Choliq, M. T., 2007, Pemodelan parameter elastic batuan degan inversi AVO untuk karak

...light (right).<ref name=Atwahetal_2021>Atwah, I., Mohammadi, S., Moldowan, M., Dahl, J., 2021. Episodic hydrocarbon charge in tight Mississippian reserv ...les from reservoirs.<ref name=Georgeetal_2007>George, S.C. Volk, H. Ahmed, M. 2007. Geochemical analysis techniques and geological applications of oil-b

...f name=pt05r8>Amaefule, J. O., Keelan, D. K., Kersey, D. G., Marschall, D. M., 1988, Reservoir description—a practical synergistic engineering and geo ...t fluid properties. Modifications of Darcy's law<ref name=pt05r119>Muskat, M., 1937, Flow of Homogeneous Fluids Through Porous Media: New York, McGraw H

...ed and [[Remote sensing|remotely sensed]],<ref name=Mayor_etal_2009>Mayor, M., S. Udry, C. Lovis, F. Pepe, D. Queloz, W. Benz, J.-L. Bertaux, F. Bouchy, ...ly different geodynamic regimes.<ref name=Dumoulin_etal_1999>Dumoulin, C., M.-P. Doin, and L. Fleitout, L., 1999, Heat transport in stagnant lid convect

| author = Daniel M. Jarvie ...drocarbons: Naturwissenschaften, v. 70, p. 133–137, doi:10.1007/BF00401597.M</ref> and secondary migration into nonsource horizons juxtaposed to the sou

...elds were discovered offshore Israel in water depths ranging from 200–1600 m (656–5249 ft). One of them, the MariB field ([[:file:M106Ch06Fig02.jpg|Fi

...ts (from vertical to horizontal wells) and of technology (from 500 to 3000 m laterals), and the Covid-19 pandemic. Nevertheless, the situation allowed c ...cales, presents a unique unconventional play, exceptionally thick (100–400 m), vast (30,000 km²), and porous (10%–20%), with a prograding c

Cooper, J.R., Godet, A., Pope, M.C., 2020. Tectonic and eustatic impact on depositional features in the uppe Corbett, K.P., Edman, J.D., Hundley-Goff, E.M., 1994. Mechanics of fracturing and faulting in the Austin Chalk-Evidence f

...e if equilibrium were established." Gaines<ref name=Gaines_1977>Gaines, A. M., 1977, Protodolomite redefined: Jour. Sed. Petrology, v. 47, p. 543-546.</

...nce method.<ref name=pt07r28>Kelley, K. R., R. W. Ward, S. Treitel, and R. M. Alford, 1976, Synthetic seismograms—a finite difference approach: Geophy

...'S''_w = 100%). This line identifies the cementation exponent (''m'') and the product of a × ''R''_''w'' (empirical constant × for ...cations_fig5.png|Figure 5]]) allow interactive parameter identification of m (the cementation exponent) and the product (''a'' × ''R''_''w'')

...s to the right of the median ([[:Image:Charles-l-vavra-john-g-kaldi-robert-m-sneider_capillary-pressure_1.jpg|Figure 1]]). We shall be concerned mostly ...01% to 99.99% is recommended ([[:Image:Charles-l-vavra-john-g-kaldi-robert-m-sneider_capillary-pressure_2.jpg|Figure 2]]).

...This is a sparsely populated area of desert and low hills, mostly 300–500 m (984–1640 ft) above sea level (msl). The highest elevation here occurs at ...ing anticlines that expose older strata. Surface elevations rise up to 850 m (2788 ft) on the Qara Chauq Dagh anticline ([[:file:M106Ch12Fig01.jpg|Figur

...tratigraphy Fifth Edition. New Jersey: Pearson Prentice Hall.</ref>defines mélange as mixed assemblage of rock consisting of brecciated blocks in a hig ...Letters, v. 37, p. 355–368.</ref> and Fein & Jurdy<ref>Fein, J. B., and D. M. Jurdy, 1986, Plate motion controls on backarc spreading: Geophysical Resea

...or offshore lease sales.<ref name=pt02r2>Capen, E. C., R. V. Clapp, and W. M. Campbell, 1971, Competitive bidding in high-risk situations: Journal of Pe

...well casing.<ref name=Chapin, David A. and Mark A. Ander>Chapin, D. A. and M. A. Ander, 1999, [http://archives.datapages.com/data/specpubs/beaumont/ch15

...mpleted using foam-based fracture treatments.<ref name=VT1993>Van Tyne, A. M., 1993, Detailed study of Devonian black shales encountered in nine wells i ...0 gal) of water and 167,800 kg (370,000 lb) of sand was used to treat a 27 m (90 ft) gross interval of the Marcellus organic shale in the Range Resource

...ically stable hydrocarbon in sedimentary basins.<ref name=ch11r16>Hunt, J. M., 1979, Petroleum Geochemistry and Geology: San Francisco, W. H. Freeman, 6

...relate well, even though they actually do not.<ref name=pt07r59>Tucker, P. M., Yorston, H. J., 1973, Pitfalls in [[Seismic interpretation]]: Tulsa, OK,

...per well for oil and between 500 and 1,500 MMscf per well for natural gas (M = 1 thousand, MM = 1 million). Initial production rates have increased over French, K.L., Birdwell, J.E. and Lewan, M.D., 2020. Trends in thermal maturity indicators for the organic sulfur-rich

...W1984 /><ref name=Peters1986 /><ref>Cooles, G. P., A. S. Mackenzie, and T. M. Quigley, 1986, Calculation of petroleum masses generated and expelled from

...g<ref name=WeimSon1989 />, Dolson et al.<ref> Dolson, J. C., D. S. Muller, M. J. Evetts, and J. Stein, 1991, [https://archives.datapages.com/data/bullet ...Fort Collins Member designated F.C.M., and Horsetooth Member designated H.M. Note perforated interval 8160–8173 ft and associated neutron-density cro

...al.,<ref name=Garciacascoetal_2006>Garcia-Casco, A., R. L. Torres-Roldan, M. A. Iturralde-Vinent, G. Millan, K. Nunez Cambra, C. Lazaro, and A. Rodrigu

...rded under exactly the same environment.<ref name=Bateman_1985>Bateman, R. M., 1985, Open-hole log analysis and formation evaluation: Boston, MA, IHRDC,

* ''M'' = gas cap size expressed as a fraction of initial reservoir oil volume; f

...tween 0.001mm and 1 mm in size) (figure 2) and nannofossils (between 5–60 μm in size). Biostratigraphy is used to identify rock formations which can occ ...the associated depositional environment.<ref name=Jenkins_2013>Jenkins, J.M. ed., 2013. Applied micropalaeontology (p. 115). Springer Science & Busines

# Schlische, R. W., M. H. Anders, 1996, Stratigraphic effects and tectonic implications of the gr

...The Leading Edge, v. 35, no. 5, p. 405-414.</ref><ref name=5Samsetal>Sams, M., P. Begg, and T. Manapov, 2017, Seismic Inversion of a Carbonate Buildup:

Being [[area::136.00 acres]] of land, more or less, a part of the M ... Russell Survey, A-12,... County, Texas, and being the same lands descri

...the [[geothermal gradient]] is [[temperature::25&deg;C]] per [[depth::1000 m]], then the pressure increase is about 1.8 psi per ft. This is more than th

...px|SEM photomicrographs of seal types.<ref name=Snider_1997>Snider, Robert M., John S. Sneider, George W. Bolger, and John W. Neasham, 1997, [http://arc

...) of the North American Mid-Continent. In shallow cores (<1000 ft, or ~300 m, deep) from east-central Iowa,<ref>Hatch, J. R., S. R. Jacobson, B. J. Witz

...ly spaced, are randomly oriented<ref name=pt08r23>Valusek, J. E., Padgett, M., Austin, J., Page, I., 1990, Zoned autopicking of seismic boosts CAEX: Oil

...l Weekly, v. 124, n. 9, p. 42-46.</ref> <ref name=Lebeaux_1952>Lebeaux, J. M., 1952, Some effects of quick-freezing upon the permeability and porosity o

...s a large effect on the [[Calculating Sw from the Archie equation|Archie ''m'' factor]] used in water saturation calculations from wireline logs and on

...of Investigations 197, 116 p.</ref><ref name=Duttn2005a>Dutton, S. P., E. M. Kim, R. F. Broadhead, C. L. Breton, W. D. Raatz, S. C. Ruppel, and C. Kera ...utton et al. <ref name=Duttn2005a /><ref name=Duttn2005b>Dutton, S. P., E. M. Kim, R. F. Broadhead, C. L. Breton, W. D. Raatz, S. C. Ruppel, and C. Kera

...oper perspective, as shown in [[:Image:Charles-l-vavra-john-g-kaldi-robert-m-sneider_capillary-pressure_5.jpg|Table 2]], which reports 1988 results by d

...s 1 and 2 of Phillip and Watson<ref name=Philip_and_Watson_1982>Philip, G. M., and D. F. Watson, 1982, A precise method for determining contoured surfac

According to Nordberg, and Cherian<ref>Nordberg, M. and M. G. Cherian, 2010, Biological responses of elements, ''in'' O. Selinus, B. ...G. Sujuan, L. Yiming, L. Chaoke, J. Rongdi, S. H. Kathleen, C. Jingxiang, M. Feng, W. Yunpeng, Y. Po, S. Shuzhuang, W. U. Frederick, W. S. Charles, and

#* '''Hydro-chloric acid solution with 0.1 M:''' If we work in carbonate fields, we need to use it to distinguish the ca