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- W2978748905 abstract "Most source rocks of the large marine oil-gas fields in domestic and overseas are graptolite shale,oil shale and marl with great amounts of clay mineral,which formed in the deepwater slope environment transferred from tableland to trough.But the carbonate rock is formed in the shallow water environment under good exchanging condition with atmosphere,which causes the low abundance of organic matter and poor-type kerogen.Hydrocarbon-expulsion efficiency of carbonate rock is lower than that of shale,and the TOC content in carbonate rock can not be reduced when the maturity increases.So,carbonate rock can not become the effective hydrocarbon source rock.The carbonate rock-argillaceous rock,limestone-siliceous shale and sea-bottom clastic rock developed from east to west in Pingliang Formation of the western Ordos Basin,which shows the lithological sequence of marine sediment resulted from increasing water depth.The graptolite shale and marl with high-abundance hydrocarbon are formed in the palaeogeographic environment of deepwater slope." @default.
- W2978748905 created "2019-10-10" @default.
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- W2978748905 date "2010-01-01" @default.
- W2978748905 modified "2023-09-24" @default.
- W2978748905 title "Development environment and lithological sequence of marine source rock:Taking Ordos Basin as an example" @default.
- W2978748905 hasPublicationYear "2010" @default.
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