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...contour map drawn on the J horizon. (c) Structure contour map drawn on the B horizon. From Yin and Groshong.<ref name=Yinandgroshong_2007>Yin, H. and R.

...84, No. 11, P. 1699–1717</ref> and modified from Balch and Hart.<ref>Hart, B. S., and Balch, R. S., 2000, Approaches to defining reservoir physical prop

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

...P''_d, the hydrocarbons will leak through the seal. If ''P''_b is less than ''P''_d, it would be possible to seal a greate :<math>P_{\rm b} = P_{\rm d}</math>

...thumb|{{figure number|1}}Relationship between the buoyancy pressure (P_b) and the capillary resistance of the water. After Berg.<ref name=ch09 ...the pore system of the aquifer as long as the [[buoyancy pressure]] (P_b) exceeds the capillary resistance of the water in the pore throats. T

...au, P. E., 2014, personal communication.</ref><ref name=Friedman>Friedman, B., 2012, [http://www.aapg.org/Publications/News/Explorer/Column/ArticleID/18

...the gravity responses (labeled A, B, and C) to a body buried to depths A, B, and C, shown in the cross section in the lower half.]] ...the gravity responses (labeled A, B, and C) to a body buried to depths A, B, and C, shown in the cross section in the lower half.

...es]] for packstones (group A) and lower resistivities for mudstones (group B), reflecting the higher water saturations of the mudstones. ...Weyburn field. Copyright: Coalson et al.;<ref name=Coalson1994>Coalson, E. B., S. M. Goolsby, and M. H. Franklin, 1994, Subtle seals and fluid-flow barr

| author = G. Yielding, B. Freeman, and D. T. Needham .../> given by fault throw divided by source-bed thickness. Methods (a) and (b) model the distance-tapering of shear-type smears, whereas method (c) model

...a/specpubs/methodo2/data/a077/a077/0001/0000/0003.htm Introduction], in L. B. Magoon and W. G. Dow, eds., The petroleum system-from source to trap: [htt ...ed gas systems: a direct type and an indirect type.<ref name=Law_2000>Law, B. E., 2000, What is a basin-centered gas system: 2000 basin-centered gas sym

...ations to fault, joints, veins, dikes, and solution surfaces, in Atkinson, B. K., ed., Fracture Mechanics of Rock: London, Academic Press, p. 277–349.

| author = G. Yielding, B. Freeman, and D. T. Needham

...> decreases and the effective size of the pore throat for oil or gas flow (B) increases.]] ...> decreases and the effective size of the pore throat for oil or gas flow (B) increases.

...ential pressure of [[pressure::4137 kPa]] (600 psi).<ref name=ch10r40>Jev, B. I., C. H. Kaars-Sijpesteign, M. P. A. M. Peters, N. W. Watts, and J. T. Wi

...e (in.) || rowspan=2 | Maximum Hole Size (in.) || colspan=5 | Mud Type^b || colspan=3 | Preferred Hole Positions || rowspan=2 | Recommended lo ! F || S || B || K || O || Excentered || Stand-Off (in.) || Centered

...f the same area shown in the upper map. The drainage areas for traps A and B were made using the migration pathway map. ...g V = A × T × Y × M. Estimation of charge volumes for the two traps (A and B) are made as follows.

...phic chart (A) correlated with a chart showing relative sea level changes (B). From Mitchum and Vail;<ref name=ch21r31 /> courtesy AAPG.]] ...chart shows the following:<ref name=ch21r31>Mitchum, R. M., P. R. Vail, J. B. Sangree, 1977, [http://archives.datapages.com/data/specpubs/seismic1/data/

...}}(a) Block diagram showing the time that Is mapped for a time slice map. (b) Interval that is mapped on time interval map. (c) Time interval map.]]

...s both traps is shown in the following figure. Trap A is at the left; trap B is at the center. ...before 100 Ma, and only a 0.2% strain that occurred 97-60 Ma. Today, trap B is a producing structure with an [[intact top seal]] capable of trapping hy

The buoyant pressure (P_b) exerted by a [[Hydrocarbon column|column of hydrocarbons]] against t :<math>\mbox{P}_{\rm b} = (\rho_{\rm w} - \rho_{\rm h}) \mbox{gh}</math>

...esidual map (A) that was calculated from the total intensity magnetic map (B). Copyright: Gay;<ref name=Gay1995>Gay, S. P., Jr., 1995, The basement faul ...esidual map (A) that was calculated from the total intensity magnetic map (B). The grid and small circles on the total intensity map are the flight path

:<math>\widehat{y} = ax + b</math> * ''b'' = y-intercept in an (x, y) coordinate system

...Al-Shaieb et al.;<ref>Al-Shaieb, Z., J. O. Puckette, A. A. Abdalla, and P. B. Ely, 1995b, [http://archives.datapages.com/data/specpubs/memoir61/ch05/006 ...Al-Shaieb et al.;<ref>Al-Shaieb, Z., J. O. Puckette, A. A. Abdalla, and P. B. Ely, 1995a, [http://archives.datapages.com/data/specpubs/memoir61/ch04/005

...ylvania, SEALS International, 4356 p.</ref><ref name=ch10r97>Yielding, G., B. Freeman, and D. T. Needham, 1997, [http://archives.datapages.com/data/bull ...m]].<ref name=ch10r13>Chong, K., P., Hoyt, P., M., Smith, J., W., Paulsen, B., Y., 1980, Effects of strain rate on oil shale fracturing: International J

| author = G. Yielding, B. Freeman, and D. T. Needham ...an otherwise shale-free sequence; Dz is the thickness of each shale bed. (b) Calculation for a sequence of reservoir zones; Dz is the thickness of each

...mann and Coalson.<ref name=Hartmannandcoalson_1990>Hartmann, D. J., and E. B. Coalson, 1990, Evaluation of the Morrow Sandstone in Sorrento field, Cheye ...mann and Coalson.<ref name=Hartmannandcoalson_1990>Hartmann, D. J., and E. B. Coalson, 1990, Evaluation of the Morrow sandstone in Sorrento field, Cheye

...of the North Sea. From Telnæs and Cooper;<ref name=ch08r53>Telnæs, N., and B. S. Cooper, 1991, Oil-source rock correlation using biological markers, Nor ...ns almost exclusively C₂₇ regular steranes (top right, peaks A, B, C).

...nited States gas production.<ref name=LawandCurtis_2002>Law, B. E., and J. B. Curtis, 2002, [http://archives.datapages.com/data/bulletns/2002/11nov/1851

...\text{A} \times \text{h} \times \Phi \times (1 - \text{S}_\text{w})}{\text{B}_\text{oi}}</math> .../ gas-oil ratio or GOR]). For example, if a well has a GOR of 1,000, then B_oi = 1.05 + (10 × 0.05) = 1.1.

...ne also ([[:file:Mth14ch02f01.jpg|Figure 1]]). Consequently, Yowlumne Unit B was created to flood the flank accumulation (Burzlaff,<ref name=Burzlaff_19 ...ape of the Yowlumne Sandstone and the relationship of Yowlumne Units A and B to the anticlinal closure.

...ed reservoir level, the field is divided into three major compartments (A, B, D) by faults. Compartment D is almost always empty, while the other compar ...he western portion of Fault A allows hydrocarbons to leak into Compartment B and then across the eastern portion of Fault A into the next highest reserv

| author = Leslie B. Magoon, Edward A. Beaumont ...role of source rock studies in petroleum exploration, in K. S. Johnson and B. J. Cardott, eds., Source Rocks in the Southern MidContinent, 1990 Symposiu

...the percentage of shale in the fault gouge.<ref name=ch10r97>Yielding, G., B. Freeman, and D. T. Needham, 1997, [http://archives.datapages.com/data/bull

Magoon and Dow<ref name=ch04r61>Magoon, L. B., and W. G. Dow, 1994, The Petroleum System--From Source to Trap: [http://s ...1 minibasin, which is bound on the north by fault A, on the east by faults B and C, and on the south by a salt-cored high. Copyright of: Armentrout et a

...structure (a) and the same structure split into 12-ms slabs and dissected (b). Suppose [[:file:interpreting-3-d-seismic-data_fig13-7.png|Figure 1]] repr ...structure (a) and the same structure split into 12-ms slabs and dissected (b). From Stark.<ref name=ch13r12 /> Courtesy SEG.]]

...,_2007b>Milani, E. J., J. H. G. Melo, P. A. Souza, L. A. Fernandes, and A. B. França, 2007b, Bacia do Paraná: Boletim de Geociências da PETROBRAS, v. ...g|Figure 2]]), according to Milani<ref name=Milani_2007a>Milani, E. J., A. B. França, and R. A. Medeiros 2007a, Rochas geradoras e rochas-reservatório

| author = Leslie B. Magoon, Edward A. Beaumont ...0339.htm Ellesmerian(!) petroleum system, North Slope, Alaska, USA], in L. B. Magoon, and W. G. Dow, eds., The Petroleum System—From Source to Trap: [

...J. F., 1988, Carbonate sequence stratigraphy, in Wilgus, C. K., Hastings, B. S., Posamentier, H. M., Van Wagoner, J., Ross, C. A., Kendall, G. C. St. C

| author = Leslie B. Magoon, Edward A. Beaumont ...bs/methodo2/data/a077/a077/0001/0000/0003.htm The petroleum system], in L. B. Magoon and W. G. Dow, eds., The Petroleum System—From Source to Trap: [h

...lbore survey calculations: Drilling-DCW, May, p. 52–59 and 118–119.</ref> (b) angle averaging method,<ref name=pt06r20 /> and (c) balanced tangential me ...ature (constant increase or decrease in deviation between survey points). (b) Minimum curvature method showing chord of single circle and the angle ϕ,

...., 10., 1016/0146-6380(86)90037-9</ref><ref name=ch08r54>Telnæs, N., Dahl, B., 1986, Oil-oil correlation using multivariate techniques: Organic Geochemi ...milarity from oil to oil. Here eight oils of type A and three oils of type B are indicated. Other geochemical evidence supports this subdivision.

...margins to retreat landward. From Hall et al.;<ref name=Hall>Hall, D. J., B. E. Bowen, R. N. Rosen, S. Wu, and A. W. Bally, 1993, Mesozoic and early Ce ===Phase B===

...hed from the mother salt. From Hall et al.;<ref name=Hall1993>Hall, D. J., B. E. Bowen, R. N. Rosen, S. Wu, and A. W. Balley, 193, Mesozoic and early Ce | B || 4–3

| author = Leslie B. Magoon, Edward A. Beaumont ...]s, [[seep]]s, or [[accumulation]]s;<ref name=Magoonanddow_1994>Magoon, L. B., and W. G. Dow, 1994, The petroleum system: From source to trap: [http://a

...and Sand B have different properties due to the presence of clays in Sand B. ...not limited to the following properties:<ref name="1Goodwayetal">Goodway, B., T. Chen, and J. Downton, 1997, Improved AVO Fluid Detection and Lithology

...rms.aspx?LookIn=term%20name&filter=oil-water%20contact oil-water contact] (B). ...g-preservation-and-destruction-of-accumulations_fig11-3.png|Figure 1 A and B]]).

...eyburn field well.<ref name=ch09r11>Coalson, E. B., D. J. Hartmann, and J. B. Thomas, 1990, Applied Petrophysics in Exploration and Exploitation: Notes ...ll in Weyburn field. From Coalson et al.;<ref name=Coalson1994>Coalson, E. B., S. M. Goolsby, and M. H. Franklin, 1994, Subtle seals and fluid-flow barr

:<math>\mbox{P}_{\rm B} = \mbox{g} \times \mbox{z} \times (\rho_{\rm w} - \rho_{\rm hc})</math> * P_B = buoyancy pressure

...² and has a volume of 450,000 km³.<ref name=Frank_2009>Frank, H. T., M. E. B. Gomes, and M. L. L. Formoso, 2009, Review of the areal extent and the volu ...cteristics:<ref name=Peate_1992 /><ref name=Nardy_2008>Nardy, A. J. R., F. B. Machado, and M. A .F. Oliveira, 2008, As rochas vulcânicas mesozoicas ác

| author = B. A. Hardage ...cal-seismic-profiles_fig3.png|{{figure number|3}}The source position (A or B) should be chosen so that the travel path to each receiver is as nearly ver

...in the Offshore Mancos Shale play. Modified from Hart<ref name=Hart>Hart, B. S., 2021, Stratigraphy and Hydrocarbon Resources of the San Juan Basin: Le ...ed) wells drilled in Mancos pools. A) In the period 2017-2020 (125 wells). B) In 2020 alone (11 wells). Contours show the top Dakota elevation, simplifi

...ation and fluids flow up the drillpipe. B is the initial flowing pressure; B′ is the final flowing pressure.

...re below approximately [[temperature::170&deg;F]]<ref name=ch11r34>Tissot, B. P., and D. H. Welte, 1984, Petroleum Formation and Occurrence, 2 ed.: New ...omatographs of a heavily biodegraded oil (A) and its undegraded precursor (B) on an example from offshore Louisiana.]]

| author = Leslie B. Magoon, Edward A. Beaumont

..., 1992, Faulting processes and fault seal, ''in'' R. M. Larsen, H. Brekke, B. T. Larsen, and E. Talleraas, eds., Structural and tectonic modelling and i ...in the rocks involved in faulting<ref name=Yieldingetal_1997>Yielding, G., B. Freeman, and D. T. Needham, 1997, [https://archives.datapages.com/data/bul

<math> R(\theta)= a\frac{\Delta Vp}{Vp}+ b \frac{\Delta \rho}{\rho}+ c \frac{\Delta Vs}{Vs} </math> where <math> a = \frac{1}{2\cos^{2}\theta}, b = 0.5-\left [ 2\left ( \frac{Vs}{Vp} \right )^{2}\sin^{2}\theta \right ], c

...ref name=ch17r75>Ruddiman, W. F., Raymo, M. E., Martinson, D. G., Clement, B. M., Backman, J., 1989, Pleistocene evolution: Northern Hemisphere ice shee ...R., E., Hetherington, E., A., Koepnick, R., B., Nelson, H., F., Otto, J., B., 1982, Variation of seawater 87Sr/86Sr throughout Phanerozoic time: Geolog

...Dolson, and M. Zinger, 1996, Gulf of Suez rift basin sequence models--Part B: Miocene sequence stratigraphy and exploration significance in the central

...160-161 ''Glob alt'' and ''Hyal B'' oils do not correlate with the Type 1-B oils<ref name=ch04r96>Thompson, K. F. M., M. C. Kennicutt II, and J. M. Bro ...of salt [[deformation]]. From Hall et al.;<ref name=Hall1993>Hall, D. J., B. E. Bowen, R. N. Rosen, S. Wu, and A. W. Bally, 1993, Mesozoic and early Ce

...ef name=AlShaieb1995a>Al-Shaieb, Z., J. O. Puckette, A. A. Abdalla, and P. B. Ely, 1995a, [http://archives.datapages.com/data/specpubs/memoir61/ch04/005 ...ref name=ch05r2>Al-Shaieb, Z., Puckette, J., O., Abdalla, A., A., Ely, P., B., 1995b, [http://archives.datapages.com/data/specpubs/memoir61/ch05/0069.ht

...als of sequence stratigraphy and key definitions, in Wilgus, C., Hastings, B., Ross, C. Posamentier, H., Van Wagoner, J., and Kendall, C. G. St. C, eds.

...ss or to establish or exercise its rights or to defend against claims and (b) when AAPG determines in its sole discretion that it is necessary to invest

...1 minibasin, which is bound on the north by fault A, on the east by faults B and C, and on the south by a salt-cored high. ...th the sediments underlying the displaced salt.<ref name=ch04r110>West, D. B., 1989, [http://archives.datapages.com/data/bulletns/1988-89/data/pg/0073/0

...Weyburn field. Copyright: Coalson et al.;<ref name=Coalson1994>Coalson, E. B., S. M. Goolsby, and M. H. Franklin, 1994, Subtle seals and fluid-flow barr ...r less), even though porosity can be as high as 30% (points 1 and 5, group B in [[:file:predicting-reservoir-system-quality-and-performance_fig9-102.png

For P ≤ P_b, use Standing correlation: For P > P_b:

...1 minibasin, which is bound on the north by fault A, on the east by faults B and C, and on the south by a salt-cored high. Copyright: Armentrout et al.; ...C. J. Travis, H. Harrison, M. R. Hudec, B. C. Vendeville, F. J. Peel, and B. F. Perkins, eds., Salt, Sediment and Hydrocarbons: Gulf Coast Section SEPM

....6 to transgressive cycles 3.7–3.8 on the Haq et al.<ref name=ch04r43>Haq, B., Hardenbol, J., Vail, P., R., 1988, Mesozoic and Cenozoic chronostratigrap ...onal extent and thickness, hydrocarbons have leaked upward into the ''Hyal B'' and ''Trim A'' reservoirs, most probably along faults during intervals of

.../> given by fault throw divided by source-bed thickness. Methods (a) and (b) model the distance-tapering of shear-type smears, whereas method (c) model ...an otherwise shale-free sequence; Dz is the thickness of each shale bed. (b) Calculation for a sequence of reservoir zones; Dz is the thickness of each

| '''Reader''' || 1 B || None || No || Read || All other readers

...tacts indicative of hydrostatic conditions in homogeneous reservoir rock. (b) Tilted, flat contacts resulting from hydrodynamic conditions. (c) Contact ...isted in Table 1 and are discussed by Bradley.<ref name=pt10r3>Bradley, H. B., ed., 1987, Petroleum Engineering Handbook: Richardson, TX, Society of Pet

...ual Research conference, p. 135–142.</ref><ref name=ch04r66>McGuinness, D. B., and J. R. Hossack, 1993, The development of allochthonous salt sheets as ...ng|{{figure number|2}}From Hall et al.<ref name=Halletal_1993>Hall, D. J., B. E. Bowen, R. N. Rosen, S. Wu, and A. W. Bally, 1993, Mesozoic and early Ce

...and compare it to published sea level cycle curves.<ref name=ch04r43>Haq, B., Hardenbol, J., Vail, P., R., 1988, Mesozoic and Cenozoic chronostratigrap ...x of the observed depositional cycles occur during the Tejas supersequence B 3.10 (0.8-0.0 Ma) third-order cycle of Haq et al.<ref name=ch04r43 />). Thi

* Kulander, B. R., S. L. Dean, and B. J. Ward, Jr., 1990, Fractured Core Analysis: Interpretation, Logging, and

...tchinson Ross, 265 p.</ref> Bolli et al.<ref name=ch17r18>Bolli, H. M., J. B. Saunders, and K. Perch-Nielsen, 1985, Plankton Stratigraphy: Cambridge, Ca ...implications for sequence stratigraphic analysis, in J. M. Armentrout, and B. F. Perkins eds., Sequence Stratigraphy as an Exploration Tool: Concepts an

....png|{{figure number|4}}Two types of flowmeters, (a) Full bore flowmeter, (b) Diverting basket type flowmeter. ...e the zones above it are all gas producers. A plug set between zones A and B will be effective at eliminating the water production in this example.

...dgers, S. Root, W. D. Lyle, D. C. Herrick, R. B. Bloch, J. W. Snedden, and B. Nwankwo, 1999, High-resolution sequence stratigraphy of a low-stand progra ...tic and upper bathyal biofacies forced basinward by falling sea level Part B is a sandstone interval map in which the biofacies excursion is less pronou

| author = Leslie B. Magoon, Edward A. Beaumont

...matter and kerogen. Definition and quantitative importance of kerogen, in B. Durand, ed., Kerogen: Insoluble Organic Matter from Sedimentary Rock: Edit .... 327, p. 52-54.</ref> (see also Tissot et al.<ref name=Tissot1987>Tissot, B. P., R. Pelet, and P. Ungerer, 1987, [http://archives.datapages.com/data/bu

...., Block, R., B., Snedden, J., W., Lyle, W., D., Herrick, D., C., Nwankwo, B., 1997, Application of high resolution biostratigraphy, Oso field, Nigeria:

...er|1}}Correlation of the third-order eustatic curve of Haq et al.<ref>Haq, B., J. Hardenbol, and P. R. Vail, 1988, Mesozoic and Cenozoic chronostratigra ...nics, climate, and sea level.<ref name=ch04r18>Beard, J., H., Sangree, J., B., Smith, L., A., 1982, [http://archives.datapages.com/data/bulletns/1982-83

| author = Leslie B. Magoon, Edward A. Beaumont ...) petroleum system in the Central Graben of the North Sea], in Magoon, L., B., Dow, W., G., eds., The Petroleum System—From Source to Trap: [http://st

...SEALS International, 4356 p.</ref><ref name=ch10r97>Yielding, G., Freeman, B., Needham, D., T., 1997, [http://archives.datapages.com/data/bulletns/1997/ ...ol. 78, no. 9, p. 1372–1385.</ref><ref name=ch10r97>Yielding, G., Freeman, B., Needham, D., T., 1997, Quantitative fault seal prediction: AAPG Bulletin,

...>\mbox{PI} = \frac{q}{\bar{p} - p_{\rm wf}} \mbox{ (for oil)} = \frac{q\mu B}{\bar{p}^{2} - p_{\rm wf}^{2}} \mbox{ (for gas)}</math> * ''B'' = formation volume factor (rcf/MSCF)

...argin Geology: AAPG Memoir 34, p. 567–581.</ref><ref name=ch04r53>Kneller, B., 1995, Beyond the turbidite paradigm: physical models for deposition of tu ...1 minibasin, which is bound on the north by fault A, on the east by faults B and C, and on the south by a salt- cored high. From Armentrout et al.;<ref>

| author = Leslie B. Magoon, Edward A. Beaumont ...petroleum occurrences are already discovered.<ref name=ch03r7>Magoon, L., B., 1995, The play that complements the petroleum system—a new exploration

| author = Leslie B. Magoon, Edward A. Beaumont

...gas produced per bbl of oil [for example, in a well with a GOR of 1000, ''B''_oi = 1.05 + (10 × 0.05)] * ''B''_gi = formation volume factor for gas at initial conditions (RES

...73, p. 613-629.</ref> and Law and Spencer<ref name=Lawandspencer_1993>Law, B. E., and C. W. Spencer, 1993, Gas in tight reservoirs-an emerging source of

...png|{{figure number|1}}Standard mudiogger's work area. (A) Chromatograph. (B) Chromatograph chart. (C) Back-up chromatograph. (D) Depth and time monitor ...number|3}}General layout of mudlogging unit. (A) Sample examination area. (B) Mudlogger's work area. (C) Sample preparation area. (Photo. Copyright: Lon

...f> Brooks et al.<ref name=ch18r9>Brooks, J., M., Kennicutt, M., C., Carey, B., D., 1986, Offshore surface geochemical exploration: Oil & Gas Journal, Oc ...radiometrics: post-survey drilling results, in Davidson, M., J., Gottlieb, B., M., eds., Unconventional Methods in Exploration for Petroleum and Natural

...ulf of Mexico. From Mitchum et al.;<ref>Mitchum, R. M., P. R. Vail, and J. B. Sangree, 1977, [http://archives.datapages.com/data/specpubs/seismic1/data/ ...pletely basinal with a slope fan overlain by shingled [[turbidite]]s. Logs B and C have deltaic and delta front sands, and midslope turbidite sands. Log

...roup), constrained by a cut-off depth of 400 m below surface<ref>Williams, B., 2019, Definition of the Beetaloo Sub basin: Northern Territory Geological ...ing: The APPEA Journal, vol. 58, no. 2, p. 799-804.</ref><ref>Altmann, C., B. Richards, A. Côté, C. Bein, E. Baruch-Jurado, and L. Jenkinson, 2020, Th

...ations, ''in'' D. S. Anderson, J. W. Robinson, J. E. Estes-Jackson, and E. B. Coalson, eds., Gas in the Rockies: Rocky Mountain Association of Geologist ...inCenteredGasFig7.jpg|{{figure number|4}}(A) Pressure and temperature and (B) vitrinite reflectance gradients for the Belco 3-28 Merna well, northern Gr

...n in stratigraphic architecture.<ref name=Dolsonetal>Dolson, J. C., Steer, B., Garing J., Osborne, G., Gad, A., and Amr, H., 1997, 3D seismic and workst ...osition II—sequence and systems tract models, in Wilgus, C., K., Hastings, B., S., Posamentier, H., W., Van Wagoner, J., Ross, C., A., Kendall, G., C.,

...ber|2}}(A) Predicted BHGM logs through a salt body in the Gulf of Mexico. (B) Model of the salt body. (C) Seismic section through the salt body. Copyrig ....png|2(C)]] is a seismic section through the salt body shown in the model (B).

...reservoir system with a strong water drive (A) and a partial water drive (B).]] ...reservoir system with a strong water drive (A) and a partial water drive (B).

...er|2}}Correlation of the third-order eustatic curve of Haq et al.<ref>Haq, B., J. Hardenbol, and P. R. Vail, 1988, Mesozoic and Cenozoic chronostratigra ...67–776.</ref><ref name=ch04r72>Pacht, J. A., B. E. Bowen, J. H. Bearn, and B. L Schaffer, 1990, Sequence stratigraphy of Plio–Pleistocene depositional

...18r15>Horvitz, L., 1969, Hydrocarbon prospecting after thirty years, in W. B. Heroy, ed., Unconventional Methods in Exploration for Petroleum and Natura ...f interest.<ref name=ch18r41>Schumacher, D., D. C. Hitzman, J. Tucker, and B. Roundtree, 1997, Applying high-resolution surface geochemistry to assess r

...Watson Wark Thomas 2006" /><ref name="Watson and Harrison 2005">Watson, E. B., & T. M. Harrison, 2005, Zircon Thermometer Reveals Minimum Melting Condit ...ystal formed.<ref name="Thomas et al. Melt Inclusions in Zircon">Thomas, J.B., R. J. Bodnar, N. Shimizu, N., & C. A. Chesner, 2003, Melt Inclusions in Z

...iety of Petroleum Engineers.</ref> and Craft et al.<ref name=pt10r7>Craft, B. C., M. Hawkins, and R. E. Terry, 1991, Applied Petroleum Reservoir Enginee The characteristic constants ''A'' and ''B'' are the corresponding slope and the intercept of the straight line obtain

...thumb|'''Figure 1.''' Wellbore diagram of (a) an open hole completion and (b) a slotted liner completion.]] ...'''Figure 2.''' Wellbore diagram of (a) a screen and liner completion and (b) a cement liner completion.]]

...compaction structures are generally found within these blocks; thus, line B or C would have found West Campbell field (WCF) but Line A would not. ...ay of connecting faults on most seismic interpretations. The connection of B to H is straightforward but, again, is diagonal to the seismic lines, where

...t'' GA-3 reservoir. Rock cutting samples from intervals indicated by A and B were used by Dow et al.<ref name=ch04r29>Dow, W. G., M. A. Yukler, J. T. Se

...leum system logic as an exploration tool in a frontier setting], ''in'' L. B. Magoon and W. G. Dow, eds., The petroleum system-from source to trap: [htt ...on || Moderate/High || Tertiary || Direct ? || Law,<ref name=Law_1996>Law, B. E., 1996, Southwestern Wyoming province (037), ''in'' D. L. Gautier, G. L.

...a fluid mobility ratio of 1.<ref name=pt10r19>Landrum, B. L., Crawford, P. B., 1960, Petroleum Transactions, AIME, v. 219, p. 407.</ref> ...ained by Craig<ref name=pt10r8 /> and Bradley.<ref name=pt10r3>Bradley, H. B., ed., 1987, Petroleum Engineering Handbook: Richardson, TX, Society of Pet

...can be significantly different for type I kerogen<ref name=ch06r13>Tissot, B., P., Pelet, R., Ungerer, P., 1987, [http://archives.datapages.com/data/bul

| author = J. M. Coleman and D. B. Prior .... The term delta was first applied by the Greek philosopher Herodotus (490 B.C.) to the triangular land surface formed by deposits from Nile River distr

...ratigraphic section above the [[source rock]].<ref name=ch04r61>Magoon, L. B., and W. G. Dow, 1994, The Petroleum System--From Source to Trap: [http://s ...alysis_fig4-45.png|{{figure number|2}}Time scale from Haq et al.;<ref>Haq, B., J. Hardenbol, and P. R. Vail, 1988, Mesozoic and Cenozoic chronostratigra

...he diffusion of low-molicular weight hydrocarbons in sedimentary rocks, in B. Doligez, ed., Migration of Hydrocarbons in Sedimentary Basins: 2nd IFP Exp

...ol. 76, p. 1000–1007.</ref><ref name=ch08r5>Chung, H. M., M. A. Rooney, M. B., Toon, G. E. Claypool, M. A. Rooney, and R. M. Squires, 1994, [http://arc

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...}}a) Inset map of the western United States showing the location of Utah. (b) Shaded relief map of Utah showing the location of the [[overthrust]] belt ...andstone. Parry, Chan, and Nash<ref name=Parry>Parry, W. T., M. A. Chan, & B. P. Nash, 2009, [http://archives.datapages.com/data/bulletns/2009/08aug/BLT

...rules is the most useful one in practice”.<ref name=ch20r242>Spalding, D., B., 1962, The art of partial modeling: 9th Symposium on Combustion, p. 833– * Spalding, D., B., 1962, The art of partial modeling: 9th Symposium on Combustion, p. 833–

* (b) technical session focused on the committee’s area of interest at an annu

...ne from the Glenn Pool data volume with sonic overlay and tracked events; (b) Horizon amplitude and time structure maps for the Wilcox. From Liner.<ref ...eismic-data_fig12-15.png|Figure 5]]. Map A uses well control only, and map B uses well control plus [[seismic interpretation]].

...umped down the inside of the drill string to the bit, surface-to-bit (s-to-b) calculations are made as follows: :<math>\mbox{S-to-b strokes} = \frac{\mbox{Total capacity in bbl}}{\mbox{pump output in bbl/st

...er the degree of fracturing, the closer the value of ''m'' is to ''m''_b. The larger the degree of fracturing, the closer the value of ''m'' i

...ample from the Frontier Sandstone, Bighorn basin, Wyoming, in Coalson, E., B., Kaplan, S., S., Keighin, C., W., Oglesby, L., A., Robinson, J., W., eds.,

...ine, vuggy, or fractured rocks. Copyright: Coalson et al.;<ref>Coalson, E. B., S. M. Goolsby, and M. H. Franklin, 1994, Subtle seals and fluid-flow barr

...ductive in the East Breaks 160-161 [[minibasin]]: ''Glob alt, Glob M, Hyal B'', and ''Trim A'' horizons. Reservoir intervals are named for the regionall ...g the ''Glob alt'' reservoir interval. Section A is uninterpreted; section B is interpreted. The reservoir thins southward between the top seal at the '

...with an example from the Frontier Sandstone, Bighorn basin, Wyoming, in E. B. Coalson, S. S. Kaplan, C. W. Keighin, L. A. Oglesby, and J. W. Robinson, e ...sity prediction using burial history. From Hayes;<ref name=Hayes>Hayes, J. B., 1983, Sandstone diagenesis as an exploration tool: AAPG Clastic Diagenesi

...calculated by using the Fréchet derivative.<ref name=Spiesandhabashy_1995>B. R. Spies and T. M. Habashy, "Sensitivity analysis of crosswell electromagn Equation (1) K_Hz = σ_b G^hz E_ϕb

Mitchum, R. M., P. R. Vail, and J. B. Sangree, 1977, [http://archives.datapages.com/data/specpubs/seismic1/data/

...ith applications to fault, joints, veins, dikes, and solution surfaces, in B. K. Atkinson, ed., Fracture Mechanics of Rock: London, Academic Press, p. 2

...e a grid of bins, each bin capturing all traces whose midpoints lie in it (B). After processing (stacking, [[Seismic migration|migration]], etc.), there

...leum source rocks by Tissot and his co-workers.<ref name=TsstWelte>Tissot, B. P., and D. H. Welte, 1984, Petroleum formation and occurrence: A new appro | B || 1.15-1.35 || 400-650 || 30-80

...ping and NW—SE strike [[thrust fault]]s along the [[Himalaya]]<ref>Upreti, B. N., 1999, An overview of the stratigraphy and tectonics of the Nepal Himal ...10, pp. 679-682.</ref><ref>Beaumont, C., R. A. Jamieson, M. H. Nguyen, and B. Lee, 2001, Himalayan tectonics explained by extrusion of a low-viscosity c

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...ure number|2}}(a) Crude base map illustrating seismic line intersections. (b) Table showing misties at seismic line intersections (times in milliseconds ...ity function of 8300 ft/sec were used, errors of +6 ft at A and -440 ft at B would appear on the depth map.

...223–238.</ref> Stahl et al.<ref name=ch18r42>Stahl, W., Faber, E., Carey, B., D., Kirksey, D., L., 1981, [http://archives.datapages.com/data/bulletns/1

...FWAL microseismograms recorded (a) at two source-receiver separations and (b) In a “soft” formation at two source-receiver separations.]] .... 274–281, DOI: 10.1190/1.1441659.</ref> <ref name=pt07r22>Hsu, K., and A. B. Baggeroer, 1986, Application of the maximum likelihood method (MLM) for so

...and accumulated in low-permeability reservoirs. Law<ref name=Law_1984>Law, B. E., 1984, Relationships of source rocks, thermal maturity, and overpressur ...ring zones, and abnormally pressured/gas-bearing zones for (A) direct and (B) indirect BCGAs.]]

| author = Leslie B. Magoon, Edward A. Beaumont ...petroleum charge, and timing. From Magoon;<ref name=Magoon1995>Magoon, L. B., 1995, The play that complements the petroleum system—a new exploration

...ure number|1}}Depositional setting of the ''Trim A'' (A) and ''Glob alt'' (B) sandstones of the East Breaks 160-161 field. After Armentrout et al.<ref n ...contrasts the depositional setting of the ''Trim A'' (A) and ''Glob alt'' (B) sandstones of the East Breaks 160-161 field. Drilling at the field encount

...and Armentrout et al.<ref name=ch04r8>Armentrout, J. M., S. J. Malacek, L. B. Fearn, C. E. Sheppard, P. H. Naylor, A. W. Miles, R. J. Desmarais, and R. ...f><ref name=ch04r72>Pacht, J., A., Bowen, B., E., Bearn, J., H., Schaffer, B., L., 1990, Sequence stratigraphy of Plio–Pleistocene depositional facies

:<math>\Phi = \frac{\rho_{\rm ma} - \rho_{\rm b}}{\rho_{\rm ma} - \rho_{\rm f}}</math> * ρ_b = formation bulk density (log value)

...px|{{figure number|1}}Wellbore diagram of (a) an open hole completion and (b) a slotted liner completion.]] ...igure number|2}}Wellbore diagram of (a) a screen and liner completion and (b) a cement liner completion.]]

...t produce variations in oil composition (Table 2<ref name=pt05r154>Tissot, B. P., and W. H. Weite, 1978, Petroleum Formation and Occurrence: New York, S ...graphic data can be displayed as chromatograms at different attenuations, (b) as star diagrams of selected peak height ratios, or (c) as data tables of

...tional systems of genetic stratigraphic units Merecure A and Oficina A and B illustrate the range of reservoir styles at Arecuna field. ====Oficina Unit B====

...ently continuous event connecting the yellow dot at A with the blue dot at B. This is a false correlation.

...mber|2}}(a) Derivative type curve used to match derivatives of test data. (b) Shapes of derivatives of test data for various reservoir conditions. ...png|{{figure number|5}}(a) Typical buildup curve shape with flow barrier, (b) Doubling of slope on Horner plot for well near barrier.

...es, the fluid spreads out on the surface and is termed '''''wetting. '''''(b) If cohesive forces exceed adhesive forces, the liquid beads up and is term ...re throat heterogeneity; the ratio of pore body to pore throat size (r_b/r_t); and the number of throats connecting each pore (coord

...ence source: New York, Springer-Verlag, 303 p.</ref><ref>Potter, P. E., J. B. Maynard, and P. J. Depetris, 2005, Mud and mudstones: Introduction and ove ...ples of pore types in mudstone. (A) and (F): pores in the mineral matrix; (B–E) and (G): pores in the organic matter. These evolutionary changes influ

...ecpubs/methodo2/data/a077/a077/0001/0200/0219.htm Hydrocarbon traps], in L.B. Magoon and W.G. Dow, eds., The Petroleum System—from Source to Trap: [ht :::b. Style (if necessary)

...preting-3-d-seismic-data_fig13-2.png|Figure 1b, c, and d]] are traverses ''b, c'', and ''d'', respectively. The fault is clearly interpretable in the ce

...2001<ref name=Sharlandetal2001>Sharland, P. R., R. Archer, D. M. Casey, R. B. Davies, S. H. Hall, A. P. Heward, et al. 2001, Arabian plate sequence stra ...-[[Mesozoic]] [[stratigraphy|stratigraphic]] column for (A) northwest and (B) east-central Saudi [[Arabian Basin]].]]

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...gure number|1}}(a) A CMP-stacked section. Copyright: a marine 3-D survey. (b) The corresponding 2-D migrated section. (c) The 3-D migrated section. (Dat ...re number|2}}(a) Selected time slices. Copyright: a marine 3-D survey and (b) a time-structure map of a marker horizon derived from the 3-D volume of mi

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...figure number|1}}From Coalson et al.<ref name=Coalsonetal_1994>Coalson, E. B., S. M. Goolsby, and M. H. Franklin, 1994, Subtle seals and fluid-flow barr

...the free-water level of a trap is tilted because the buoyant force (P_b) is interfered with by the hydrodynamic force (P_w). The re

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...imestones of the Lodgepole Formation (<ref name=GaswirthMarra>Gaswirth, S. B. and K. R. Marra, 2015, U.S. Geological Survey 2013 assessment of undiscove Garcia-Fresca et al.<ref name=Garciaetal>Garcia-Fresca, B., D. Pinkston, R. G. Loucks, and R. LeFever, The Three Forks playa lake dep

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| author = J. B. Thomas ...ods_fig6.png|{{figure number|6}}(a) X-ray fluoroscopy slab photograph and (b) plane light slab photograph of a Pennsylvanian sandstone from Oklahoma.

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...n, P. Weimer, A. Lowrie, H. W. Pettingill, R. L. Phair, H. H. Roberts, and B. Van Hoorn, eds., Petroleum systems of deep-water basins: Global and Gulf o ...as. From Beaubouef.<ref name=Beaubouef1999>Beaubouef, R. T., C. Rossen, F. B. Zelt, M. D. Sullivan, D. C. Mohrig, and G. D. C. Jennette, 1999, Field gui

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..., showing the expression of faults. In the left map, locations ''a'' and ''b'' show strong gradients, which indicate faults. A series of truncated trend

...g rock stress (from Amadei & Stephanson<ref name=AmadeiStephansson>Amadei, B., and O. Stephansson, 1997, Rock stress and its measurement: Amsterdam, Net ...med|center|{{figure number|7}}(a) The principal stresses acting on a cube (b) Mohr Circles in three dimensions.]]

...replacement is distance, rotation as an angle move.<ref name=Ralph>Ralph, B., 1998, Basic Vibration Theory: London.</ref> ...e reliable method.<ref name=Ariadji_et_al>Ariadji, T., H. Purwanto, and D. B. Scarboroug, 2005, Metode Peramalan Dan Evaluasi Keekonomian Teknologi Vibr

...of demonstrating connection.<ref name=ch17r6>Azevedo, D., F. Aquino Mato, B. Simoneit, and A. Pinto, 1992, Novel series of tricyclic aromatic terpanes

...urface-maps_fig4.png|300px|thumb|{{figure number|4}}(a) Cross section and (b) net pay Isopach map of the Strachan gas field, western Canada. Contour Int ...e-1987-36-peh Development plan for oil and gas reservoirs], in Bradley, H. B., ed., Petroleum Engineering Handbook: Richardson, TX, Society of Petroleum

...y) and then follows the fracture gradient.<ref name=pt03r8>Barker, C., and B. Horsfeld, 1982, [http://archives.datapages.com/data/bulletns/1982-83/data/ ...ric logs of two wells offshore Louisiana. Well A had normal pressure. Well B, 2000 ft away and across a growth fault, showed a sudden decrease in resist

...e length with the deformed line length between two arbitrary points, A and B. In this figure, 1₀ is the initial, undeformed line length; 1<su

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

...<ref name=Bautistaetal2015>Bautista, D., E. Vaz dos santos Neto, and H. de B. Penteado, 2015, Control son Petroleum composition of the Llanos Basin, Col ...roleum province]]s (Doligez et al., 1986<ref name=Doligezetal1986>Doligez, B., F. Bessis, J. Burrus, Ph. Ungerer, and P. Y. Chenet, 1986, Integrated num

...Report 5, p. 75– 123.</ref> showing topset, foreset, and bottomset beds; (B) Deltaic and neritic facies from Frazier<ref>Frazier, D. E., 1967, Recent d * Baganz, O. W., B. Yuval, B. Kevin, and N. Dag, 2012, Lacustrine Sandstone Reservoirs and Hydrocarbon S

Graphic correlation<ref name=ch17r79>Shaw, A., B., 1964, Time in Stratigraphy: New York, McGraw-Hill, 365 p.</ref> is a wide

...he same surface data. (a) Unconstrained extrapolation into nondata areas. (b) Contours constrained to areas near data.]] ...average algorithm tend to “come back” to the average of near data values. (b) Acceptable surface extrapolation achieved by creating a first-order trend,

...gridge and Smith,<ref name=Morgridgeandsmith_1972>Morgridge, D. L., and W. B. Smith Jr., 1972, [http://archives.datapages.com/data/specpubs/fieldst4/dat ...> Lawton et al.,<ref name=Lawtonetal_1987>Lawton, T. F., G. W. Geehan, and B. J. Voorhees, 1987, Lithofacies and depositional environments of the Ivisha

...displacement pressure.<ref name=ch10r1>Alger, R. P., D. L. Luffel, and R. B. Truman, 1989, New unified method of integrating core capillary pressure da

...it by a factor that converts P_c to [[buoyancy pressure]] (P_b). If the conversion factor is not known, we use 0.4 for gas and 0.7 f

...d silt-laminae of the Mowry Shale throughout Wyoming<ref>Anderson, A., and B. Kowallis, 2005, Storm deposited fish debris in the Cretaceous Mowry Shale ...oxide storage resources: U.S. Geological Survey Open-File Report 2012–1024–B, 30 p.

...S, M. Mbadinga, Y. F. Liu, S. Z. Yang, J. F. Liu, R. Q. Ye, J. D. Gu, and B. Z. Mu, 2015, [https://www.nature.com/articles/srep09801 Insights into the .... 11, no. 2, p. 188-194.</ref><ref name="10Bolletal">Boll, M., C. Loffler, B. E. Morris, and J. W. Kung, 2014, [https://sfamjournals.onlinelibrary.wiley

...e-stimulation practices in Jonah field, Sublett County, Wyoming, ''in'' E. B. Coalson, J. C. Osmond, and E. T. Williams, eds., Innovative applications o ...ations, ''in'' D. S. Anderson, J. W. Robinson, J. E. Estes-Jackson, and E. B. Coalson, eds., Gas in the Rockies: Rocky Mountain Association of Geologist

...availability of the desired acreage by (a) examining the public records, (b) reviewing notices of lease sales, (c) making local inquiries, and (d) obse

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...sonable representation of the structural configuration for the basin. Part B shows migration pathways from the Bakken, based on the basin structural con

...tom samples from the present-day [[Gulf of Mexico]]. Similar analyses of ''B. alhatrossi'' specimens from Neogene sections can be compared with the mode

...] trap (A, at t = 1) is juxtaposed against a sandstone at some later time (B, at t = 2). This probably will result in rapid spillage. If further fault m

| author = J. M. Coleman and D. B. Prior ...Mississippi River delta.<ref name=Colemanetal_1981>Coleman, J. M., and D. B. Prior, 1981, [http://archives.datapages.com/data/specpubs/sandsto2/data/a0

...(a) CMP stack showing reffections from a salt dome in the Gulf of Mexico. (b) Stack after DMO processing. Steep portions of diffractions and reflections seismic-migration_fig6.png|{{figure number|6}}(a) Unmigrated and (b) migrated stack of DMO-processed data from the Gulf of Mexico.

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...992>Moldowan, J. M., C. Y. Lee, P. Sundararaman, T. Salvatori, A. Alajbeg, B. Gjukic, G. J. Demaison, N. E. Slougue, and D. S. Watt, 1992, Source correl

...rs. Deeper infiltration occurs from (a) eustatic sea level changes and/or (b) tectonic elevation of basin margins.

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...#Jackups|jackup rigs]], the [http://www.glossary.oilfield.slb.com/en/Terms/b/blowout_preventer.aspx blowout preventers] (BOPs) are mounted above sea lev ...{figure number|3}}Semisubmersible rigs, (a) Pontoon type semisubmersible. (b) Twin hull semisubmersible. From Whittaker.<ref name=pt03r50 />

...er|1}}Location of Weyburn field. Copyright: Coalson et al.<ref>Coalson, E. B., S. M. Goolsby, and M. H. Franklin, 1994, Subtle seals and fluid-flow barr

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...rajectory_fig6.png|{{figure number|6}}(a) Steerable bottom hole assembly, (b) Kicking off with a bent sub and straight mud motor.]] ...e-trajectory_fig7.png|{{figure number|7}}(a) Packed bottom hole assembly, (b) Fulcrum effect for build angle.]]

| SPOT || 60 × 60 || 20 (color), 10 (b&w)

...string. (a) Typical MFE inflate open hole string (straddle, off-bottom). (b) Typical MFE straddle string (open hole, conventional, off-bottom). (From F ...e located inside and above the closing tool. (A) Add cushion/run in hole; (B) initial flow period; (C) initial shut-in period; (D) final flow period; (E

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...al fluid contents from reservoir to surface. (a)Oil-productive formation. (b) Gas-productive formation. (Courtesy of Core Laboratories, a Division of We ...tic lose about 30% of their water in 3 days.<ref name=Auman_1989>Auman, J. B., 1989, A laboratory evaluation of core preservation materials: SPE Formati

* Time B is the highstand of sea level and represents advanced progradation. Updip,

...mann and Coalson.<ref name=Hartmannandcoalson_1990>Hartmann, D. J., and E. B. Coalson, 1990, Evaluation of the Morrow sandstone in Sorrento field, Cheye

====Stage B==== The two continents, separated in Stages A and B now collide. The remnant ocean basin is completely subducted. Technically t

...in the Tertiary Niger Delta in west Africa.<ref name=Evamyetal_1978>Evamy, B. D., J. Haremboure, P. Kamerling, W. A. Knaap, F. A. Molloy, and P. H. Rowl ...ributary channel fills.<ref name=Richardsonetal_1989>Richardson, J. G., J. B. Sangree, and R. M. Sneider, 1989, Sand-rich deltas: Journal of Petroleum T

where P_b is the buoyancy pressure; ρ_w and ρ_nw are the ...or of an oil column. Redrawn from Jennings,<ref name=Jennings>Jennings, J. B., 1987, [http://archives.datapages.com/data/bulletns/1986-87/data/pg/0071/0

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...disappear altogether along another northwest-trending line farther east (B–B′). This may be a strike-slip fault, which is not common in this area, or ...ghs and lows and along truncation lines of anomalies. On the right figure (b), two faults located from subsurface mapping are shown, labeled U/D. The ev

file:fishing_fig7.png|{{figure number|7}}(a) Tapered mill, (b) Flat mill.

...3–236.</ref><ref name=Delisleetal_2010>Delisle, G., M. Teschner, E. Faber, B. Panahi, I. Guliev, and C. Aliev, 2010, [http://archives.datapages.com/data ...ref name=Wieneretal_2010>Wiener, R. W., M. G. Mann, M. T. Angelich, and J. B. Molyneux, 2010, [http://archives.datapages.com/data/specpubs/memoir93/CHAP

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:<math>M = \frac{\Delta t_{\rm fl} - \Delta t_{\rm log}}{\rho_{\rm b} - \rho_{\rm fl}} \times 0.01</math> :<math>N = \frac{\phi_{N{\rm fl}} - \phi_{N\log}}{\rho_{\rm b} - \rho_{\rm fl}}</math>

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...}}Typical models used in reservoir simulation. (a) Zero-dimensional tank. (b) One-dimensional linear. (c) One-dimensional radial. (d) Two-dimensional cr ...2.png|thumb|300px|{{figure number|2}}(a) Pseudo-relative permeability and (b) capillary pressure curves calculated for two-layer thicknesses compared to

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| author = J. M. Coleman and D. B. Prior ...(a) the inertia of the issuing water and associated turbulent diffusion; (b) friction between the effluent and the bed just seaward of the mouth; and (

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...x|{{figure number|1}}Various types of seismic displays: (a) wiggle trace, (b) variable area, (c) variable area wiggle trace, and (d) variable density. C

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...|1}}Wireline formation tester. (a) Retracted configuration (tool closed). (b) Set configuration (tool set).

...of square kilometers.<ref name=Richardsonetal_1988a>Richardson, J. G., J. B. Sangree, and R. M. Sneider, 1988, Eolian dunes: Journal of Petroleum Techn Ciftci et al.<ref name=Ciftcietal_2004>Ciftci, B. N., A. A. Aviantara, N. F. Hurley, and D. R. Kerr, 2004, [http://archives.

...al environments and reservoir compartmentalization within the Frio zone 21-B reservoir, Tijerina-Canales-Blucher field, South Texas (abs.): Transactions Richardson et al.<ref>Richardson, J. G., J. B. Sangree, and R. M. Sneider, 1988, Coastal barrier reservoirs: Journal of P

...increased production ([[:file:M125-WattenbergField-Figure3.jpg|Figure 3A, B]]). ...menced in 2010. The addition of new horizons contributes to field growth. (B) Production curve for horizontal wells for Wattenberg Field. Modern horizon

...y contrast (A), while trough-going joints formed at low rigidity contrast (B). Illustration of different join patterns (C and D), as bed contained forme

...|thumb|300px|{{figure number|4}}Schematic diagram of (a) steady-state and (b) unsteady-state apparatus.]] ...pressures || Measures additional reservoir description parameters: β and ''b''

...l Resolution || Radius of Investigation || Applications || Limitations^b ^b<sub>The ohm-meter (Ω-m) is a unit of measurement of resistance.</sub

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* ''Option B'' The solution to the problem shown in Figure 1 is option B. It is the preferred choice because it has the higher estimated present val

...png|{{figure number|3}}Histograms showing (a) average porosity values and (b) average permeability values for cored tight gas reservoir facies. (From Mo

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...oduction decreased from peak rates in 1971 to a low of 2000 BOPD in 1994. (b) Well activity by year in the South Pass 62 field. Dark gray bars indicate

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:<math>y = ax + b</math> **''b'' = constant (range) value ([[:log-analysis-applications_fig3.png|Figure 3]

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...section]] of subduction zone consisting three zonations of deformation: a, b, and c. This classification is based on deformation mechanism and materials ...hic bulge, causing regional positive [[gravity]] anomaly of +500 gu. Zone ‘b’ is the contact of oceanic and continental crust. Compressive forces are

...dles include (a) unrealistically high DCFROR or corporate discount rates, (b) overly cautious cost estimates, and (c) overly pessimistic wellhead price

...ata-acquisition-on-land_fig5.png|{{figure number|5}}(a) Off end shooting. (b) Split spread shooting.

...y (London) Special Publication 15, p. 3–16.</ref><ref name=Flmng>Flemming, B. W., 2000, A revised textural classification of gravel-free muddy sediments ...e (after Lazar et al. <ref name=Lzrea2015a />): (A) texture (grain size); (B) bedding; (C) composition (OMA = organo-mineralic aggregate); (D) organic m

...on dioxide capture and storage, prepared by Working Group III of the IPCC (B. Metz, O. Davidson, H. C. de Connick, M. Loos, and L. A. Meyer, eds): New Y ...s, v. 8, no. 3, p. 166–176.</ref><ref name=Bradshawetal_2002>Bradshaw, J., B. E. Bradshaw, G. Allinson, A. J. Rigg, V. Nguyen, and L. Spencer, 2002, The

...rmation of fracture and oil charging, well LJ1, 3470.40 m (11,382.91 ft). (B) Two-phase aqueous fluid inclusions (yellow arrows) present in pre-TSR calc ...r|2}}Carbonate classification schemes of (a) Folk<ref name=pt05r56 /> and (b) Dunham,<ref name=pt05r50 /> both based on textures observed in hand specim

...hor = P. J. Hicks Jr., C. M. Fraticelli, J. D. Shosa, M. J. Hardy, and M. B. Townsley ...ealizations. (A) Results without filtering based on the calibration data. (B) Results with filtering based on the calibration data.

...art of the basin, Niobrara reservoir targets are the chalks, named, the C, B, and A from bottom to top. The top of the Niobrara sits unconformably on th

...nalysis similar to that of Winland, Franklin<ref name=ch09r12>Coalson, E., B., Goolsby, S., M., Franklin, M., H., 1994, Subtle seals and fluid-flow barr

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* Bodet, L., P. Cobbold, O. Galland, J.-B. Gressier, J.-Y. Matthieu, and R. Mourgues, 2010, Control of pore fluid pre

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