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- W747415028 abstract "The average content of organic carbon in the Domanik-like formations is more than 0.5%, and that of the sub-Domanik is from 0.1 to 0.5%. Among both these types there are varieties in which several percent organic carbon is present in the rock. Abundance of carbonaceous material in the section increased from early to middle Riphean time and then dropped off. This abundance again increased in Vendian time to reach maximum at the beginning of the Cambrian. These units extended over almost all the Siberian platform. However, in the Upper Cambrian they are restricted to the north of the platform, and in the Ordovician and Silurian to the west." @default.
- W747415028 created "2016-06-24" @default.
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- W747415028 date "1982-01-01" @default.
- W747415028 modified "2023-09-27" @default.
- W747415028 title "Carbonaceous Sedimentary Rocks of the Upper Precambrian and Lower Paleozoic of the Siberian Platform" @default.
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