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  • * [[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

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