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  • ...and [[sporinite]]; common but not restricted to [[marine]] settings; Type II pathway on [[Van Krevelen diagram]]s.<ref name=Petersetal_2012>Peters, Kenn
    1 KB (181 words) - 21:10, 6 July 2015

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  • ...oil]] at a lower [[thermal maturation|thermal maturity]] than typical type II kerogens with less than 6 wt. % sulfur;<ref name=Orr_1986>Orr, W. L., 1986, * [[Type II kerogen]]
    1 KB (205 words) - 21:10, 6 July 2015
  • ...pted to classify [[kerogen]] types [[Type I kerogen|I]], [[Type II kerogen|II]], [[Type III kerogen|III]], and [[Type IV kerogen|IV]]. More common is the
    1 KB (194 words) - 15:46, 8 March 2016
  • ...elow for [[Rock-Eval pyrolysis]] T<sub>max</sub> for [[Kerogen types|types II and III kerogens]]. Different pyrolysis techniques have different cutoffs f | Oil (from type II kerogen) || 435–455
    3 KB (411 words) - 21:19, 9 February 2022
  • ...generation]] zones, maturity, and transformation ratio for standard types II and III kerogens, based on a specific burial and thermal history model. The ! [[vitrinite reflectance|Vitrinite refl.]], % R<sub>o</sub>, Type II
    4 KB (503 words) - 14:18, 14 February 2022
  • | II || Rocks with pores capable of producing gas with natural or artificial fra The table below lists the characteristics of pore types I, II, and III.
    6 KB (882 words) - 17:19, 6 April 2022
  • * [[Type II kerogen]]
    1 KB (176 words) - 21:06, 6 July 2015
  • * [[Type II kerogen]]
    1 KB (185 words) - 21:11, 6 July 2015
  • ...and [[sporinite]]; common but not restricted to [[marine]] settings; Type II pathway on [[Van Krevelen diagram]]s.<ref name=Petersetal_2012>Peters, Kenn
    1 KB (181 words) - 21:10, 6 July 2015
  • * [[Type II kerogen]]
    1 KB (180 words) - 21:11, 6 July 2015
  • ...ogen]] defines the kerogen as type [[Type I kerogen|I]], [[Type II kerogen|II]], or [[Type III kerogen|III]] and if the rock will be oil or gas prone.
    3 KB (525 words) - 18:09, 9 February 2022
  • ...this generality applies only if a [[source rock]] is composed of pure type II organic matter (marine kerogen).
    2 KB (220 words) - 16:10, 10 February 2022
  • ...II kerogen makes it more gas and condensate prone than the shallower, Type II kerogen Niobrara. The prevalence of several shallower, oilier reservoirs ab * Craddock, W. H., R. M. Drake II, J. C. Mars, M. D. Merrill, P. D. Warwick, M. S. Blondes, M. A. Gosai, et.
    4 KB (677 words) - 17:14, 22 December 2023
  • | [[Type II kerogen|II]] ...generation]] zones, maturity, and transformation ratio for standard types II and III kerogens, based on a specific burial and thermal history model. The
    17 KB (2,363 words) - 17:40, 9 February 2022
  • ...px|thumb|{{figure number|1}}Typical gas chromatogram examples for types I, II, and III kerogen.]] ...from the sample's kerogen. Typical gas chromatogram examples for types I, II, and III kerogen are shown in [[:file:evaluating-source-rocks_fig6-5.png|Fi
    6 KB (817 words) - 18:19, 9 February 2022
  • ...300px|thumb|{{figure number|1}}Approximate boundaries for kerogen types I, II, and III. Copyright: Tissot and Welte;<ref>Tissot, B. P., and D.H. Welte, 1 ...ig6-7.png|Figure 1]] shows the approximate boundaries for kerogen types I, II, and III. Time-temperature relationships and mixing of various sources of o
    7 KB (970 words) - 14:28, 10 February 2022
  • ...W. G., M. A. Yukler, J. T. Senftle, M. C. Kennicutt, and J. M. Armentrout II, 1990, Miocene oil source beds in the East Breaks basin, Flex-Trend, offsho ...es.<ref name=ch04r96>Thompson, K. F. M., M. C. Kennicutt, and J. M. Brooks II, 1990, [http://archives.datapages.com/data/bulletns/1990-91/data/pg/0074/00
    6 KB (850 words) - 15:33, 23 March 2022
  • * Family II: microcrystalline allochemical limestone that consists of > 10% allochems w Family I and II of Folk’s system could be subdivided based on the type of allochems prese
    16 KB (1,986 words) - 14:09, 19 December 2023
  • ...tion|hydrocarbon-generation]] zones are greater for type III than for type II kerogen. Therefore, a trend is only valid if based on analysis of samples f
    3 KB (421 words) - 18:26, 9 February 2022
  • | Indirect || liquid-prone types I/II kerogen || <0.1 || short/long || over-/underpressure || thermal [[cracking]
    4 KB (469 words) - 19:01, 14 March 2016
  • ...ith the Type 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-
    7 KB (1,080 words) - 17:44, 23 March 2022
  • *High Fe(II), Ni(II), Co(II) content quenches CL.
    11 KB (1,477 words) - 15:25, 24 January 2022
  • .... The Ek2 shale is in overall good-very good source rock containing Type I-II kerogen, in average of 3.6% TOC, and at the oil-mature stage with 0.68% to ...The lacustrine Shahejie shale contains 1.5-19.6% TOC in general of Type I-II organic matter origin and mainly at the immature to high mature stage up to
    8 KB (1,251 words) - 15:51, 14 March 2022
  • ...trital inputs. Kerogen is mainly represented by oil-prone Type II and Type II-S (French et al.<ref name=French>French, K. L., J. E. Birdwell, and M. D. L
    11 KB (1,594 words) - 19:15, 8 February 2024
  • ...ts. The organic matter is mainly represented by oil-prone Type II and Type II-S kerogens (French et al., 2020 and references therein). Production trends
    10 KB (1,550 words) - 21:50, 3 March 2022
  • ...re was a fall in the oil prices which eventually picked up after World War II. The war caused a disruption in the supply of the oil which caused a market
    6 KB (926 words) - 19:38, 14 March 2019
  • ..., which average approximately 11% total organic carbon and consist of type-II kerogen. The primary reservoir targets are low-porosity and low-permeabilit | Kerogen Type || Type II
    11 KB (1,595 words) - 20:20, 2 June 2021
  • ...Brasileira de Geociências, São Paulo, v. 18, p. 172-190</ref> The Gondwana II supersequence of the Paraná Basin, restricted to occurrences in Rio Grande ...erregional character. These are the Rio Ivaí, Paraná, Gondwana I, Gondwana II, Gondwana III and Bauru.
    22 KB (3,382 words) - 19:52, 4 January 2024
  • ...tier, H. W., and P. R. Vail, 1988, Eustatic controls on clastic deposition II—sequence and systems tract models: SEPM Special Publication 42, p. 125– .../0073/0002/0100/0143.htm Genetic stratigraphic sequences in basin analysis II: application to northwest Gulf of Mexico Cenozoic basin]: AAPG Bulletin, vo
    7 KB (901 words) - 20:45, 22 February 2022
  • ...and shaly sandstones, including both low-quality reservoir rocks and Type II-III source rocks. As such, it is best described as a hybrid play.
    6 KB (985 words) - 20:14, 2 June 2021
  • ...lls: Proceedings of the Third World Petroleum Congress, The Hague, Section II, p. 503–521.</ref> infers the true reservoir pressure by extrapolating th
    6 KB (997 words) - 17:55, 17 February 2022
  • ...ced the bullet gun, which was the main perforating tool prior to World War II.
    19 KB (2,910 words) - 21:06, 18 January 2022
  • ...3% to 2.98% and mean value is 0.44% ± 0.36%. It contains a mixture of type II and type III kerogen. Mean Tmax value is 444.138°C. ...5% to 10.82% and mean value is 3.5% ± 2.55%. It contains a mixture of type II and type III kerogen. Mean Tmax value is 442.249°C.
    52 KB (7,769 words) - 20:28, 18 January 2017
  • ...Colorado, "in" N. H. Foster and E. A. Beaumont, eds., Stratigraphic traps II: AAPG Treatise of Petroleum Geology, Atlas of Oil and Gas Fields, p. 305–
    7 KB (1,044 words) - 16:57, 13 April 2022
  • ...hich average approximately 11% total organic carbon (TOC) and contain Type II kerogen. The primary reservoir targets are the low porosity and low permeab
    7 KB (1,004 words) - 22:08, 4 March 2022
  • ==Phase II== ...lves into underpressured conditions. Both systems, subsequent to the phase II history of overpressure, may experience a period of uplift and erosional un
    34 KB (4,772 words) - 14:44, 12 March 2019
  • ...ormity (after Faqira et al., 2009<ref name=Faqiraetal2009 />). MA-I and MA-II show the two areas selected for a 2-D basin modeling study. The [[Unayzah]] ...mp, 1999<ref name=Jonesandstump1999 />). This hot shale unit contains type II amorphous organic matter, with [[graptolite]] and [[chitinozoan]]s, and ran
    18 KB (2,569 words) - 22:50, 8 January 2019
  • ...ganic matter components. These four types have evolved to kerogen types I, II, III,<ref name=TsstWelte /> and IV. These narrowly defined kerogen types ar ...mblages with H/C values of 0.8 might contain some oil-generative type I or II kerogen with predominantly inert type IV kerogen or might contain all gas-g
    17 KB (2,472 words) - 17:39, 13 April 2022
  • ...hemistry, organic matter in the New Albany Shale belongs to oil-prone type II kerogen, but petrographic studies suggest that it is composed of organic ma
    7 KB (1,107 words) - 21:50, 4 March 2022
  • | II || About the same as the overlying unit || Increase or decrease; may change
    9 KB (1,404 words) - 21:39, 27 March 2019
  • ...ntina], ''in'' O. R. Berg and D. G. Woolverton, eds., Seismic Stratigraphy II: An integrated approach to hydrocarbon exploration: [http://store.aapg.org/ ...sudoriental del Engolfamiento Neuquino. XII Congreso Geológico Argentino y II Congreso de Exploración y Desarrollo de Hidrocarburos, Actas I, p. 382-394
    16 KB (2,490 words) - 15:32, 8 January 2021
  • ...eds., Unconventional Methods in Exploration for Petroleum and Natural Gas II: Dallas, Southern Methodist Univ. Press, p. 116–123.</ref>
    10 KB (1,443 words) - 16:08, 25 January 2022
  • ...Magnus field], in E. A. Beaumont and N. H. Foster, eds., Structural traps: II. Traps associated with tectonic faulting: Treatise of petroleum geology of ...simulation modeling of the 100-foot channel complex, Texas, and the Ainsa II channel complex, Spain: Analogs to multistory and multilateral channelized
    20 KB (2,850 words) - 15:33, 15 January 2024
  • ...er small distances. Sampson<ref name=pt08r19>Sampson, R. J., 1978, Surface II graphics system (revision 1): Lawrence, KS, Kansas Geological Survey, Serie ...is an evaluation of mapping packages.<ref name=pt08r7>Geobyte, 1986, CEED II—mapping systems compared, evaluated: Geobyte, v. 1, n. 5, p. 25–40.</re
    25 KB (3,597 words) - 20:49, 19 January 2022
  • ...ciclastic facies, where the TOC ranges 5 to 20% and kerogen is mostly type II. The Cenomanian-Turonian Eagle Ford- Tuscaloosa super sequence has black sh .... TOC content ranges from less than 2% up to 8% and kerogen is mostly type II with a type III contribution.<ref name=Guptaetal_2017>Gupta, I., Rai, C., S
    27 KB (3,791 words) - 19:35, 11 October 2022
  • ...dell, including Confluence Resources, Mallard Exploration, Bison Oil & Gas II, Edge Energy, Boomtown, and Clear Creek Resource Partners.
    9 KB (1,412 words) - 21:46, 3 March 2022
  • ...: Dow et al.;<ref>Dow, W. G., M. A. Yukler, J. T. Senftle, M. C. Kennicutt II, and J. M. Armentrout, 1990, Miocene oil source beds in the East Breaks bas
    11 KB (1,482 words) - 15:47, 21 March 2022
  • .../0073/0002/0100/0143.htm Genetic stratigraphic sequences in basin analysis II: application to northwest Gulf of Mexico Cenozoic basin]: AAPG Bulletin, vo
    14 KB (1,901 words) - 15:16, 9 January 2024
  • ...L. W. Teufel, 1985, A comprehensive fracture diagnostics experiment, Part II, Comparison of seven fracture azimuth measurements: Society of Petroleum En
    13 KB (1,964 words) - 20:50, 19 January 2022
  • * Ettre LS, Sakodynskii KI. M. S. Tswett and the discovery of chromatography II: Completion of the development of chromatography (1903-1910). Chromatograph
    15 KB (2,280 words) - 21:00, 21 April 2022
  • One can also define a distance ''d''<sub>ii&prime;</sub> between any two variables ''x''<sub>''i''</sub> and ''x''<sub>
    16 KB (2,349 words) - 15:46, 19 January 2022
  • | OMT lower Miocene source (type II %/type III %)<sup>2</sup> || 50/50 || 90/10 || 100/0 | OMT other 2 sources (type II %/type III %)<sup>2</sup> || 80/20 || 90/10 || 100/0
    38 KB (5,890 words) - 15:16, 23 August 2016
  • ...with increasing angle), whereas under wet condition, both sands have class II AVO (dim amplitude at Near and Far angle). It should be noted that differen
    15 KB (2,356 words) - 18:00, 26 April 2022
  • ...tions: American Association of Landmen Comprehensive Land Practices, Chap. II, p. 1-13.</ref> provide a summary of pertinent information related to land
    15 KB (2,269 words) - 19:25, 19 January 2022
  • ...esolution, surface-sensitive (topographic) information of the sample. Type II secondary electrons (SE2), however, are generated from a deeper and wider v
    16 KB (2,441 words) - 20:24, 23 January 2019
  • * Crans, W., Mandl, G., 1980, On the theory of growth faulting; part II (a): genesis of the “unit”: Journal of Petroleum Geology, vol. 3, p. 20
    16 KB (2,083 words) - 21:28, 2 February 2022
  • ...trital grains. (B) Dolomite overgrowths. (C) Fibrous (three phases i.e. I, II and III) and medium-coarse crystalline (MD) dolomite cements associated wit Morrow, D.W., 1982b. Diagenesis II. Dolomite – part II. Dolomitization models and ancient dolostones. Geoscience Canada, 9, 95-107
    38 KB (4,996 words) - 21:07, 21 April 2022
  • ...of gas. The [[Silurian]] and Upper [[Cretaceous]] sections, rich in [[type II kerogen]], form the [[source rock]]s for the petroleum and gas in these bas
    17 KB (2,361 words) - 16:19, 30 January 2017
  • ...the transformation of oil to gas in indirect systems (initiation of phase II on [[:file:BasinCenteredGasFig1.jpg|Figure 2]]) is uncertain. Conventional
    20 KB (2,949 words) - 18:24, 6 April 2016
  • ...Versickerung und Anwendung auf die Bewasserung): S.-Ber. Wiener Akad. Abt. II a, v. 136, p. 271–306.</ref> which considered the porous media as a bundl
    19 KB (2,716 words) - 19:02, 20 January 2022
  • ...s on wettability and relative permeabilities of carbonate reservoir rocks: II: Energy Sources, v. 7(1), no. 7, p. 67–75.</ref> The degree of wettabilit
    22 KB (3,508 words) - 20:34, 3 March 2016
  • | Log curves || LAS or LIS-II
    19 KB (2,872 words) - 14:28, 20 January 2022
  • ...ths, and P. F. Worthington, eds., Geological application of wire-line logs II: Geological Society Special Publication 65, p. 141–154.</ref>
    43 KB (6,686 words) - 13:44, 18 March 2019
  • ...SA]: AAPG Bulletin, v. 82, p. 412-441.</ref> The Utica Shale contains type II kerogen and is thermally overmature (>1.3% R<sub>o</sub>).
    25 KB (3,445 words) - 19:01, 14 March 2016
  • ...ization of smectite and the precipitation of [[quartz]], ankerite and type II calcite cements. In addition to the increase in temperature and pressure, t
    27 KB (3,802 words) - 19:32, 9 January 2024
  • * Are marine shales commonly described as type II organic matter (HIo: 250–800 mg/g) .../> and a comparable issue exists for organic matter categorized as a type II marine shale.
    73 KB (10,728 words) - 18:16, 11 January 2024
  • ...enberg is 200 to 250 ft (>2 wt.% TOC). The source beds are dominantly Type II with some Type III kerogen present. The source beds are all marine Type II kerogen with admixtures of Type III. This type of source bed can generate b
    72 KB (10,249 words) - 20:06, 15 January 2024
  • .... The gases produced in other areas show a thermogenic marine origin (type II kerogen), with a lower contribution of biogenic methane<ref name=Brssn2020> ...racteristics ([[:file:M125-VacaMuerta-Figure16.jpeg|16A]] and window I and II in ([[:file:M125-VacaMuerta-Figure16.jpeg|Figure 16B]]). Although the dista
    77 KB (11,201 words) - 20:07, 15 January 2024
  • | Indirect || liquid-prone types I/II kerogen || <0.1 || short/long || over-/underpressure || thermal [[cracking]
    34 KB (5,070 words) - 15:11, 23 August 2016
  • ...1968, Introduction to paleolimnology: in Developments in sedimentology, v. II: Amsterdam, Elsevier, 228 p.
    33 KB (4,905 words) - 16:40, 6 April 2016
  • ...like transitions of sills to hypsometric levels observed in profiles (i), (ii), and (iii). The figure is from Magee et al., 2016]]
    29 KB (4,365 words) - 21:07, 21 April 2022
  • ...ncept, in J. R. Paterson and J. R. Laurie, eds., Cambro–Ordovician studies II: Memoirs of the Association of Australasian Palaeontologists 32, p. 247–2
    58 KB (8,121 words) - 16:35, 1 August 2016
  • ...otidal river channel: Ord River, Western Australia: Estuarine Research, v. II: New York, Academic Press, p. 309-321.</ref>
    60 KB (9,022 words) - 17:17, 21 March 2016
  • ...rboniferous stratigraphy, facies patterns and palaeogeography of Iran Part II. Northern and central Iran: Acta Geologica Polonica, v. 55, no. 1, p. 31–
    79 KB (11,542 words) - 18:47, 19 July 2016
  • ...t Siberian Basin.<ref name=Lptn2003 /> The Bazhenov Shale is a marine type II kerogen that is the primary source rock in the West Siberian Basin, with TO
    97 KB (14,873 words) - 19:53, 11 January 2024
  • ...It traps nitrosamines in the digestive tract to cancel any chance of type II diabetes. Due to its negative charge, zeolite can attract toxins such as he
    83 KB (12,860 words) - 14:03, 10 April 2019
  • ...iscovery subpeak years occurred during and immediately after the World War II, with 1957 being the last year, which had cumulative reserve discoveries of
    157 KB (23,278 words) - 18:36, 16 January 2024