51. Paleoenvironment of the Lower–Middle Cambrian Evaporite Series in the Tarim Basin and Its Impact on the Organic Matter Enrichment of Shallow Water Source Rocks
- Author
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Wei Liu, Mingyang Wei, Hua Zhang, Zheng Shen, G. Harrison, Kai Lu, Zhidong Bao, Xiting Xu, Demin Zhang, Axel Munnecke, and Zongfeng Li
- Subjects
paleoenvironment ,Evaporite ,Lower–Middle Cambrian ,0211 other engineering and technologies ,Geochemistry ,02 engineering and technology ,evaporite series ,010502 geochemistry & geophysics ,01 natural sciences ,ddc:551 ,Organic matter ,021108 energy ,0105 earth and related environmental sciences ,chemistry.chemical_classification ,Total organic carbon ,Tarim Basin ,Geology ,Geotechnical Engineering and Engineering Geology ,Mineralogy ,Anoxic waters ,shallow water source rock ,Waves and shallow water ,chemistry ,Source rock ,Paleosalinity ,Sedimentary rock ,QE351-399.2 - Abstract
Just as in deep-water sedimentary environments, productive source rocks can be developed in an evaporitic platform, where claystones are interbedded with evaporites and carbonates. However, the impact of the paleoenvironment on the organic matter enrichment of shallow water source rocks in an evaporite series has not been well explored. In this study, two wells in the central uplift of the Tarim Basin were systematically sampled and analyzed for a basic geochemical study, including major elements, trace elements, and total organic carbon (TOC), to understand the relationship between TOC and the paleoenvironmental parameters, such as paleosalinity, redox, paleoclimate, paleo-seawater depth, and paleoproductivity. The results show that the Lower–Middle Cambrian mainly developed in a fluctuating salinity, weak anoxic to anoxic, continuous dry and hot, and proper shallow water environment. The interfingering section of evaporites, carbonates, and claystones of the Awatag Fm. have higher paleoproductivity and higher enrichment of organic matter. Paleosalinity, redox, paleoclimate, paleo-seawater depth, and paleoproductivity jointly control the organic matter enrichment of shallow water source rocks in the evaporite series. The degree of enrichment of organic matter in shallow water source rocks first increases and then decreases with the increase in paleosalinity. All the samples with high content of organic matter come from the shallower environment of the Awatag Fm.
- Published
- 2021
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