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

  • * [[Palynofacies and kerogen analysis]]
    4 KB (493 words) - 20:00, 31 January 2022
  • ...res are supplied with full-spectrum hydrocarbons migrating directly from [[kerogen]] in contact with the pores. Larger shale pores are also preferentially sup ...eded before hydrocarbons can migrate from the [[source rock]]. Sorption by kerogen is dominant over that of mineral phases.
    8 KB (1,133 words) - 15:16, 14 February 2022
  • * [[Palynofacies and kerogen analysis]]
    4 KB (483 words) - 15:15, 31 January 2022
  • ...)]] contained in a rock. Quality is measured by determining the types of [[kerogen]] contained in the organic matter. Thermal maturity is most often estimated
    4 KB (569 words) - 21:38, 4 February 2022
  • ...istry, organic matter in the New Albany Shale belongs to oil-prone type II kerogen, but petrographic studies suggest that it is composed of organic matter of ...pper Devonian New Albany Shale during thermal maturation: Implications for kerogen transformation, in W. Camp, K. Milliken, K. Taylor, N. Fishman, P. Hackley,
    7 KB (1,107 words) - 21:50, 4 March 2022
  • ...s to [[Source rock|source]] variations.<ref name=ch08r36>Orr, W. L., 1986, Kerogen/asphaltene/sulfur relationships in sulfur-rich Monterey oils: Organic Geoch
    4 KB (571 words) - 17:34, 15 February 2022
  • ...icles on [[Paleoclimatology]], [[Paleobathymetry]], and [[Palynofacies and kerogen analysis]]). * [[Palynofacies and kerogen analysis]]
    10 KB (1,252 words) - 19:55, 31 January 2022
  • ...originate mainly from higher plants and consist of type III (gas-prone) [[kerogen]] dominated by [[Thermal maturation#Vitrinite|vitrinite]] group [[maceral]]
    5 KB (737 words) - 14:52, 15 August 2016
  • Hydrocarbon types reflect the composition of the [[kerogen]]s from which they were generated. Kerogens are the insoluble organic matte
    5 KB (633 words) - 20:02, 18 February 2022
  • #* ''Y'' = hydrocarbon yield per volume of source from each [[kerogen]] facies and maturity class
    6 KB (834 words) - 20:41, 14 February 2022
  • ...of factors that include compaction, chemical reactions, source richness, [[kerogen]] type, and thermal expansion. [[Petroleum generation|Hydrocarbon generati
    6 KB (828 words) - 16:32, 4 April 2022
  • ...hich average approximately 11% total organic carbon and consist of type-II kerogen. The primary reservoir targets are low-porosity and low-permeability member | Kerogen Type || Type II
    11 KB (1,595 words) - 20:20, 2 June 2021
  • ...ntary rock that contains a high proportion of endogenous organic matter ([[kerogen]]) mostly insoluble in ordinary petroleum solvents, from which substantial
    6 KB (893 words) - 19:01, 14 March 2016
  • ...shape. To date, analysis of particle images has been applied largely to [[kerogen]] particles in transmitted, reflected, and fluorescent light. The results s
    5 KB (718 words) - 20:59, 31 January 2022
  • ...tion SEPM 9th Annual Research conference, p. 139–150.</ref> to calibrate [[kerogen]] type for kinetic [[modeling]].
    6 KB (850 words) - 15:33, 23 March 2022
  • ...ratures necessary for [[cracking]] kerogens into hydrocarbons. (See also [[Kerogen type and hydrocarbon generation]].)
    6 KB (929 words) - 19:41, 22 March 2022
  • ...nic matter and structured algal palynomorphs are associated with oil-prone kerogen. Palynology, in integration with other disciplines also can help to assess
    14 KB (1,899 words) - 21:03, 21 April 2022
  • ...h average approximately 11% total organic carbon (TOC) and contain Type II kerogen. The primary reservoir targets are the low porosity and low permeability me
    7 KB (1,004 words) - 22:08, 4 March 2022
  • ...0.14% to 0.38% and the mean is 0.25% ± 0.09%. This level contains type III kerogen and mean Tmax value is 455.44 °C. ...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.
    52 KB (7,769 words) - 20:28, 18 January 2017
  • * [[Palynofacies and kerogen analysis]]
    7 KB (921 words) - 18:09, 24 January 2022
  • ...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
  • ...irectly related to porosity development resulting from the conversion of [[kerogen]] to hydrocarbons.
    89 KB (13,415 words) - 19:16, 16 January 2024

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