Cited by 56Hydrocarbon exploration and reservoir analysisGeochemistry and Elemental AnalysisPaleontology and Stratigraphy of Fossils

Diagenesis, Catagenesis and Metagenesis of Organic Matter

Tissot, Bernard P., Welte, Dietrich H.·1984·Petroleum Formation and Occurrence

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Crossref · 10.1007/978-3-642-87813-8_6

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  • If hopanes and steranes in metamorphosed Archean rocks are syngenetic, they survived burial temperatures well above the oil window, about 150 °C.

    “the discovery of hopanes and steranes in metamorphosed Archean rocks requires that, if these carbon skeletons are syngenetic, then they have persisted despite experiencing prolonged burial temperatures well above the end of the oil window (∼150 °C)”

    From Reappraisal of hydrocarbon biomarkers in Archean rocks (2015) · cites this paper as [12]

  • At a vitrinite reflectance of 2% and an H/C ratio of 0.5, catagenesis transitions into metagenesis, the dry gas zone where only methane is generated.

    “At a vitrinite reflectance of 2% and H/C ratio of 0.5, catagenesis transitions into metagenesis, which corresponds to the dry gas zone where only methane is generated (12,36).”

    From Reappraisal of hydrocarbon biomarkers in Archean rocks (2015) · cites this paper as [12]

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Authors
Tissot, B. P., & Welte, D. H.
Affiliations
  • IFP Énergies nouvelles (FR)
  • Forschungszentrum Jülich (DE)
Venue
Petroleum Formation and Occurrence
Published
1984
Pages
69-73
OpenAlex
W1485386798
Cited by
56
References
0
Citations by year
2026: 1 · 2025: 7 · 2024: 3 · 2023: 5 · 2022: 4 · 2021: 6 · 2020: 4 · 2019: 5 · 2018: 10 · 2017: 1 · 2015: 2 · 2012: 1
FWCI
0.00
Type
book chapter
Language
en
Open access
closed
Locations
Springer eBooks (publishedVersion)
Topics
  • Physical Sciences › Engineering › Mechanics of Materials › Hydrocarbon exploration and reservoir analysis
  • Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
  • Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
Keywords
diagenesis, catagenesis, metagenesis, organic matter transformation, sedimentary basins, organic-inorganic interactions, early diagenesis, mineral composition, pore water, organic liquids, thermal maturation, biological activity

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