湘西北奥陶系宝塔组灰岩龟裂纹构造特征、成因及其资源意义

黄乐清; 刘伟; 柏道远; 李泽泓; 梁恩云; 陈珍宝

doi:10.3799/dqkx.2018.123

Volume 44 Issue 2

Feb. 2019

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Article Navigation > Earth Science > 2019 > 44(2): 399-414

Huang Leqing, Liu Wei, Bai Daoyuan, Li Zehong, Liang Enyun, Chen Zhenbao, 2019. Characteristics, Petrogenesis and Resource Significance of the Limestone with Polygonal Reticulate Structure of Pagoda Formation, in Northwestern Hunan Province. Earth Science, 44(2): 399-414. doi: 10.3799/dqkx.2018.123

Citation:

Huang Leqing, Liu Wei, Bai Daoyuan, Li Zehong, Liang Enyun, Chen Zhenbao, 2019. Characteristics, Petrogenesis and Resource Significance of the Limestone with Polygonal Reticulate Structure of Pagoda Formation, in Northwestern Hunan Province. Earth Science, 44(2): 399-414. doi: 10.3799/dqkx.2018.123

Citation:

Huang Leqing, Liu Wei, Bai Daoyuan, Li Zehong, Liang Enyun, Chen Zhenbao, 2019. Characteristics, Petrogenesis and Resource Significance of the Limestone with Polygonal Reticulate Structure of Pagoda Formation, in Northwestern Hunan Province. Earth Science, 44(2): 399-414. doi: 10.3799/dqkx.2018.123

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Characteristics, Petrogenesis and Resource Significance of the Limestone with Polygonal Reticulate Structure of Pagoda Formation, in Northwestern Hunan Province

doi: 10.3799/dqkx.2018.123

Hunan Institute of Geology Survey, Changsha 410116, China

Received Date: 2018-12-30
Publish Date: 2019-02-15

Abstract

Abstract

The limestone of the upper Ordovician Baota Formation in northwestern Hunan has a crack structure, bearing the characteristics of "decreasing cracks from top-bottom, no crossing between adjacent layers, multi-period deformation, water-like filling" in rock sequence, which is a special sedimentary structure in geological period. In order to find out its genetic mechanism and its internal relationship with the evolution of the Yangtze basin, the author does research from aspects including lithology, fracture characteristics, geochemical characteristics, basin model and comprehensive comparison of the known causes of crack-like polygonal reticulate structure. It is found that the crack structure is a kind of initial slit formed under the influence pen contemporaneous gel condensation. Then under the control of tectonic extrusion, the basin sinks rapidly, a fluid environment in an abnormal high pressure filed is formed in the basin, which leads to squeezing, filling and initial cracks reconstruction from the plaster material in underlying water-rich rocks. This study on the crack structure of the Baota Formation provides petrological data for the study on the mechanism of tectonic-fluid-rock interaction. Meanwhile, a good dredging function of the cracks has an important practical significance for the study on mineralization as well as oil and gas accumulation.
- polygonal reticulate structure,
- Baota Formation,
- formation mechanism,
- Ordovician,
- Northwestern Hunan Province,
- rock

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References(90)

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Characteristics, Petrogenesis and Resource Significance of the Limestone with Polygonal Reticulate Structure of Pagoda Formation, in Northwestern Hunan Province

doi: 10.3799/dqkx.2018.123

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