Search results

• Basin modeling: identifying and quantifying significant uncertainties
  | OMT lower Miocene source (type II %/type III %)² || 50/50 || 90/10 || 100/0 | OMT other 2 sources (type II %/type III %)² || 80/20 || 90/10 || 100/0
  38 KB (5,890 words) - 15:16, 23 August 2016
• Rock physics analysis for reservoir identification
  ...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
• Land description and maps
  ...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
• Scanning electron microscopy (SEM)
  ...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
• Tectonic modeling
  * 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
• Dolomite and dolomitization: Implications for reservoir characterization
  ...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
• Libya hydrocarbon provinces
  ...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
• Basin-centered gas systems: elements and processes
  ...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
• Permeability
  ...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
• Reservoir fluids
  ...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
• Geology workstation
  | Log curves || LAS or LIS-II
  19 KB (2,872 words) - 14:28, 20 January 2022
• Data: sources
  ...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
• Basin-centered gas systems: examples
  ...SA]: AAPG Bulletin, v. 82, p. 412-441.</ref> The Utica Shale contains type II kerogen and is thermally overmature (>1.3% R_o).
  25 KB (3,445 words) - 19:01, 14 March 2016
• Sandstone sedimentology and stratigraphy
  ...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
• Shale-gas resource systems
  * 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
• Wattenberg field
  ...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
• Vaca Muerta play
  .... 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
• Basin-centered gas systems: evaluation and exploration strategies
  | 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
• Delta plain, upper
  ...1968, Introduction to paleolimnology: in Developments in sedimentology, v. II: Amsterdam, Elsevier, 228 p.
  33 KB (4,905 words) - 16:40, 6 April 2016
• Sill intrusion mechanism, parameters, and temperature effect of sills on a petroleum system
  ...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

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