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- W2374720152 abstract "Carbonate cement is the product from activity of palaeo fluids,containing much profitable geological information on diagenetic environment and diagenetic fluid evolution. In this paper,integrating methods of petrology,mineralogy and geochemistry,the origin mechanism of carbonate cements are investigated in Eboliang structure belt,northern margin of Qaidam Basin. The result shows that the major carbonate cements are calcite and Fe-bearing calcite in the study area. The calcite cements are mainly discovered in Eboliang structure I,their carbon and oxygen isotope values have wide range(-13. 47‰δ13CPDB2. 54‰,-15. 93‰δ18OPDB-4. 74‰) and varied origin,such as organic matter decarboxylation,syngenetic or parasyngenetic,bacterial methanogenesis. However,The Fe-bearing calcite cements are maily discovered in Eboliang structure III and Yahu structure,the distribution of carbon and oxygen isotope values concentrates at-4. 24‰δ13CPDB-1. 99‰,-11. 17‰δ18OPDB-9. 41‰, precipitated from sedimentary compacted water. The carbonate cements origin reveals the information on interaction between inorganic and organic fluid activity in Eboliang structure belt,which provides the important evidence for the hydrocarbon accumulation study in this area." @default.
- W2374720152 created "2016-06-24" @default.
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- W2374720152 date "2015-01-01" @default.
- W2374720152 modified "2023-09-23" @default.
- W2374720152 title "Origin of Carbonate Cements in Reservoir Rocks and Its Petroleum Geologic Significance: Eboliang structure belt,northern margin of Qaidam Basin" @default.
- W2374720152 hasPublicationYear "2015" @default.
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