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    Late Paleozoic subsidence and burial history of the Fort Worth basin: Discussion (2019)
    American Association of Petroleum Geologists (AAPG)
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    Publication Date: 2019
    Description: 〈span〉〈a href="https://pubs.geoscienceworld.org/aapgbull#b1"〉Alsalem et al. (2017)〈/a〉 present a burial history model for a well in the Fort Worth basin showing 3.7–5.2 km (2.3–3 mi) of burial during the Pennsylvanian. The generalized burial history diagram in their figure 5 suggests that vitrinite reflectance (%〈span〉R〈/span〉〈sub〉〈span〉o〈/span〉〈/sub〉) varies linearly with depth, or nearly so, and that %〈span〉R〈/span〉〈sub〉〈span〉o〈/span〉〈/sub〉 values in the Barnett Shale are related primarily to depth of burial. Their modeling results indicate that the maturity of the Barnett Shale is caused by approximately 4.5 km (∼2.8 mi) of burial. 〈a href="https://pubs.geoscienceworld.org/aapgbull#b1"〉Alsalem et al. (2017)〈/a〉 do not consider any driving mechanisms for increased maturity, except heat flow through the lithosphere. If other sources of heat affected maturity values measured on organic material in the Barnett Shale, then their burial history curves would need to be modified accordingly.〈/span〉
    Print ISSN: 0149-1423
    Electronic ISSN: 1943-2674
    Topics: Geosciences
    Published by American Association of Petroleum Geologists (AAPG)
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