四川盆地西南中二叠统白云岩的地球化学特征及其成因

韩晓涛; 鲍征宇; 谢淑云

doi:10.3799/dqkx.2016.013

Volume 41 Issue 1

Jan. 2016

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Article Navigation > Earth Science > 2016 > 41(1): 167-176

Han Xiaotao, Bao Zhengyu, Xie Shuyun, 2016. Origin and Geochemical Characteristics of Dolomites in the Middle Permian Formation, SW Sichuan Basin, China. Earth Science, 41(1): 167-176. doi: 10.3799/dqkx.2016.013

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Han Xiaotao, Bao Zhengyu, Xie Shuyun, 2016. Origin and Geochemical Characteristics of Dolomites in the Middle Permian Formation, SW Sichuan Basin, China. Earth Science, 41(1): 167-176. doi: 10.3799/dqkx.2016.013

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Origin and Geochemical Characteristics of Dolomites in the Middle Permian Formation, SW Sichuan Basin, China

doi: 10.3799/dqkx.2016.013

Han Xiaotao^{1,2
,},
Bao Zhengyu^{1,2
,
,},
Xie Shuyun^1,3

1.
Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2.
Liaoning Institute of Geology and Mineral Resources, Shenyang 110032, China
3.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China

Received Date: 2015-08-10
Publish Date: 2016-01-15

Abstract

Abstract

The dolomite reservoir plays an important role in the research of carbonate oil and gas reservoirs. The origin of dolomite is an integral component in analyzing the evolution of pore-cave-fracture system in high-quality dolomite reservoirs. The dolomites of Middle Permian Qixia Formation, SW Sichuan basin were studied in this paper by the method of petrology and geochemical analyses aiming at the discovery of the origin of dolomites. The dolomites are mainly controlled by fault zones, associated with zebra fabric. The dolomite fabrics exhibit non-planar saddle crystals and strongly undulose extinctions. In addition, the high degree of order is found in hydrothermal dolomites. The geochemical characteristics of saddle dolomites show noticeable negative δ¹⁸O_PDB and an enrichment of strontium isotopes. In the end, the dolomites have been proved to be the product of structurally controlled hydrothermal dolomitization on the basis of comprehensive geologic research.
- SW of Sichuan basin,
- Middle Permian,
- Qixia Formation,
- hydrothermal dolomite,
- geochemistry

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References(50)

References

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Origin and Geochemical Characteristics of Dolomites in the Middle Permian Formation, SW Sichuan Basin, China

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