thermal_maturity
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thermal_maturity [10/05/2023 16:35] – mike_gss | thermal_maturity [11/05/2023 09:25] (current) – mike_gss | ||
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//Inputs into Petroleum Systems Analysis.// | //Inputs into Petroleum Systems Analysis.// | ||
- | Most source-rocks are marine in origin although coals and certain lacustrine sediments can also be very organic rich. Some of the most prolific source-rocks (grouped by age) are listed below: | + | Most source-rocks are marine in origin although coals and certain lacustrine sediments can also be very organic rich. Some of the world' |
* **Silurian** (9%); Qusaiba and correlatives, | * **Silurian** (9%); Qusaiba and correlatives, | ||
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* **Oligocene-Holocene** (13%); Maykop, Eastern Paratethys - accounts for much of oil and gas in South Caspian (Miocene Diatom Suite also a contributor) | * **Oligocene-Holocene** (13%); Maykop, Eastern Paratethys - accounts for much of oil and gas in South Caspian (Miocene Diatom Suite also a contributor) | ||
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thermal_maturity.1683736511.txt.gz · Last modified: 10/05/2023 16:35 by mike_gss