四川盆地北缘五峰组和龙马溪组沉积构造格局研究

肖斌; 刘树根; 冉波; 李智武; 叶玥豪; 韩雨樾

doi:10.3799/dqkx.2020.208

Volume 46 Issue 7

Jul. 2021

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Article Navigation > Earth Science > 2021 > 46(7): 2449-2465

Xiao Bin, Liu Shugen, Ran Bo, Li Zhiwu, Ye Yuehao, Han Yuyue, 2021. Study on Sedimentary Tectonic Pattern of Wufeng Formation and Longmaxi Formation in the Northern Margin of Sichuan Basin, South China. Earth Science, 46(7): 2449-2465. doi: 10.3799/dqkx.2020.208

Citation:

Xiao Bin, Liu Shugen, Ran Bo, Li Zhiwu, Ye Yuehao, Han Yuyue, 2021. Study on Sedimentary Tectonic Pattern of Wufeng Formation and Longmaxi Formation in the Northern Margin of Sichuan Basin, South China. Earth Science, 46(7): 2449-2465. doi: 10.3799/dqkx.2020.208

Citation:

Xiao Bin, Liu Shugen, Ran Bo, Li Zhiwu, Ye Yuehao, Han Yuyue, 2021. Study on Sedimentary Tectonic Pattern of Wufeng Formation and Longmaxi Formation in the Northern Margin of Sichuan Basin, South China. Earth Science, 46(7): 2449-2465. doi: 10.3799/dqkx.2020.208

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Study on Sedimentary Tectonic Pattern of Wufeng Formation and Longmaxi Formation in the Northern Margin of Sichuan Basin, South China

doi: 10.3799/dqkx.2020.208

Xiao Bin^{1, 2
,
,},
Liu Shugen^{2, 3
,
,
,},
Ran Bo²,
Li Zhiwu²,
Ye Yuehao²,
Han Yuyue²

1.
Mining Institute of Liaoning Technical University, Fuxin 123032, China
2.
State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, China
3.
School of Energy and Power Engineering, Xihua University, Chengdu 610039, China

Received Date: 2020-07-14
Publish Date: 2021-07-15

Abstract

Abstract

In order to reconstruct the sedimentary tectonic pattern of Wufeng Formation and Longmaxi Formation in the northern margin of Sichuan Basin, the Wufeng Formation and Longmaxi Formation in the Micangshan-Dabashan area of the northern margin of Sichuan Basin were taken as the research objects. The stratigraphic framework correlation and sedimentary facies analysis were carried out, and Mo/TOC and Al-Co[EF]×Mn[EF] geochemical indicators were used to determine the degree of water mass restricted in the sedimentary period. It is found that near the uplift area, controlled by the material supply and sedimentary space, the thickness of strata varies greatly, and the thickness of black shale is smaller as a whole. However, far away from the uplift area, the black shale gradually thickens from west to east and the TOC content increases under the control of the upwelling at the continental margin and intracontinental depression.Research shows that: (1) The Wufeng Formation in Micangshan area was deposited in Fucheng of Nanzheng County, and Qiaoting of Nanjiang County, in the intersection area of two kinds of upwelling currents, which were influenced by the upwelling currents for a long time. The sedimentary period of Longmaxi Formation was mainly influenced by the Xixiang Rise, which resulted in the uplift of Wangcang and Nanjiang areas into islands, with the thickest deposition in Well Mashen 1. (2) Generally, the Wufeng Formation in the Dabashan front and the western Hubei-eastern Chongqing area presents a pattern of uplift-depression alternation. Due to the continuous compression of the Cathaysian block from SE to NW, the Shizhu-Wuxi line subsided continuously during the sedimentary period of the Longmaxi Formation, resulting in a relatively thick stratigraphic deposition.
- Wufeng Formation,
- Longmaxi Formation,
- upwelling currents,
- sedimentary tectonic pattern,
- Sichuan Basin,
- tectonics

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References(65)

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Study on Sedimentary Tectonic Pattern of Wufeng Formation and Longmaxi Formation in the Northern Margin of Sichuan Basin, South China

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