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There is a page named "Kerogen" on this wiki. See also the other search results found.

  • ...ansgressive shales are organic rich and buried in the thermal regime for [[kerogen]] [[cracking]], hydrocarbons will be generated. If the [[lithofacies]] form
    9 KB (1,239 words) - 16:58, 24 February 2022
  • ...s source rock Vaca Muerta Formation (2-9% TOC, hi-quality oil-prone marine kerogen) and the Early Cretaceous Agrio Formation (TOC 2%–5%). Superimposed petro ...carbonate and some siliciclastic facies, where the TOC ranges 5 to 20% and kerogen is mostly type II. The Cenomanian-Turonian Eagle Ford- Tuscaloosa super seq
    27 KB (3,791 words) - 19:35, 11 October 2022
  • * kerogen http://www.thefreedictionary.com/kerogen
    22 KB (3,024 words) - 21:42, 19 December 2014
  • ...he 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 1.16% Ro
    8 KB (1,251 words) - 15:51, 14 March 2022
  • ...c rocks—even those at a grade high enough to contain graphite instead of [[kerogen]] (R<sub>0</sub> > 8%). For example the Shell Barret #1 well in Hill County
    11 KB (1,525 words) - 18:50, 1 February 2022
  • ...nd Rock Springs formations. Organic matter is largely gas-prone type III [[kerogen]]<ref name=Law_1984 /> with additional contribution from thermally cracked ...: 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
  • ...rogen content or organic [[maceral]] percentages from chemical or visual [[kerogen]] assessments. As TOC values vary throughout a source rock because of organ ...f values, and that all generate more oil than gas from primary cracking of kerogen. TOC = total organic carbon.
    73 KB (10,728 words) - 18:16, 11 January 2024
  • ...ve been affected by localized depositional conditions and detrital inputs. Kerogen is mainly represented by oil-prone Type II and Type II-S (French et al.<ref
    11 KB (1,594 words) - 19:15, 8 February 2024
  • | Direct || gas-prone type III [[kerogen]] || <0.1 || short || over-/underpressure || hydrocarbon generation || capi | Indirect || liquid-prone types I/II kerogen || <0.1 || short/long || over-/underpressure || thermal [[cracking]] of oil
    34 KB (5,070 words) - 15:11, 23 August 2016
  • * [[Palynofacies and kerogen analysis]]
    11 KB (1,595 words) - 18:09, 24 January 2022
  • ...nt amounts of free oil to produce, but must be heated to generate oil from kerogen either in the subsurface or after mining and retorting. This 2d part of cha ...127 p.</ref><ref>L. Wenger, 2010, personal communication</ref> likely from kerogen diagenesis. The release of CO2 also explains the apparent increase in hydro
    97 KB (14,873 words) - 19:53, 11 January 2024
  • ...source rock samples varies from −27.5 to −26 PDB (average −26.4) for the [[kerogen]], and from −28 to −26, (average −26.6) for the extracted bitumen. Th
    27 KB (3,901 words) - 13:51, 26 January 2017
  • ...layers of [[Siliceous_microfossils#Radiolarians|siliceous radiolaria]], [[kerogen]], and fish debris. This mudstone was deposited in a restricted basin, wher
    17 KB (2,331 words) - 20:11, 10 August 2016
  • * [[Palynofacies and kerogen analysis]]
    16 KB (2,247 words) - 19:23, 24 January 2022
  • ...gas. The [[Silurian]] and Upper [[Cretaceous]] sections, rich in [[type II kerogen]], form the [[source rock]]s for the petroleum and gas in these basins.
    17 KB (2,361 words) - 16:19, 30 January 2017
  • ...en 10 nm and 100 μm, and are present both in kerogen and bitumen. In turn, kerogen and bitumen fill the interparticle and intraparticle pores (as well as natu ...ation; VCARB = volume of carbonate; VCL = volume of clay; VKER = volume of kerogen; VQFP = volume of quartz, feldspar, and plagioclase (modified from Ortiz et
    77 KB (11,201 words) - 20:07, 15 January 2024
  • ...value and evaluated permeability of velocity flow of fluids, water, and [[kerogen]]. The result will show linear tred of diagram Kf vs saturation. It also de
    29 KB (4,601 words) - 16:09, 12 April 2016
  • ...t (>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 both oil
    72 KB (10,249 words) - 20:06, 15 January 2024
  • ...rogen in the process of conversion to oil verses updip nonthermally mature kerogen in a nonporous, nonproductive mudrock. Examples are the Sanish and Parshall ...igh pressure because of the maturation and conversion of organic material (kerogen) to hydrocarbons. Those hydrocarbons are trapped in an increasing pressure,
    157 KB (23,278 words) - 18:36, 16 January 2024
  • ...il. This is because they can be particularly rich in [[coal]]s and woody [[kerogen]], which form gas-prone humic source material. Gas fields are found in the
    34 KB (4,776 words) - 18:18, 5 January 2024

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