Geochemical Classification and Significance of Jurassic CoalBearing Source Rocks in Taibei Depression, TurpanHami Basin
- Received Date: 1900-01-01
- Rev Recd Date: 1900-01-01
- Publish Date: 2010-12-10
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Key words:
- TurpanHami Basin /
- coalbearing source rocks /
- biomarkers index /
- type of source rock
Abstract: The sedimentary environments and the original inputs of source rocks close related with the nature of the organic matter, in different layers and different regions of Taibei Depression, TurpanHami Basin, due to the differences of the depositional environments and the original inputs of Jurassic coalbearing source rocks, result in differences of the geochemical index. The analysis of geochemical indicators of source rocks showing that Pr/Ph and C29ααα20R relative content are important indicators of redox environment and the salinity of water. At the same time, we found that the main indicators of the type of source rocks are aromatic hydrocarbon and asphaltene contents in the group composition of soluble organic matter, the ratio of saturated hydrocarbon and aromatic hydrocarbon ,also the ratio of nonhydrocarbon and asphaltene. Pr/Ph, gammacerane index are secondary indicators of classification of source rocks. The Jurassic coalbearing source rocks can be classfied into three categories by the above index in Taibei Depression.
Citation: | WANG Zhiyong. Geochemical Classification and Significance of Jurassic CoalBearing Source Rocks in Taibei Depression, TurpanHami Basin[J]. Acta Sedimentologica Sinica, 2010, 28(6): 1238-1243. |