Diagenesis, Catagenesis and Metagenesis of Organic Matter
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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
- Publisher
- Springer Berlin Heidelberg
- 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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