川东北通南巴背斜中新生代构造变形的砂箱构造物理模拟

马德龙; 王宏斌; 张希晨; 何登发; 凡睿; 王彦君; 黄林军; 崔键; 刘文强; 杨秀磊

doi:10.3799/dqkx.2022.423

Volume 48 Issue 4

Apr. 2023

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Article Navigation > Earth Science > 2023 > 48(4): 1307-1320

Ma Delong, Wang Hongbin, Zhang Xichen, He Dengfa, Fan Rui, Wang Yanjun, Huang Linjun, Cui Jian, Liu Wenqiang, Yang Xiulei, 2023. Analogue Modeling of Structural Deformation of Tongnanba Anticline in Mesozoic and Cenozoic, NE Sichuan Basin. Earth Science, 48(4): 1307-1320. doi: 10.3799/dqkx.2022.423

Citation:

Ma Delong, Wang Hongbin, Zhang Xichen, He Dengfa, Fan Rui, Wang Yanjun, Huang Linjun, Cui Jian, Liu Wenqiang, Yang Xiulei, 2023. Analogue Modeling of Structural Deformation of Tongnanba Anticline in Mesozoic and Cenozoic, NE Sichuan Basin. Earth Science, 48(4): 1307-1320. doi: 10.3799/dqkx.2022.423

Citation:

Ma Delong, Wang Hongbin, Zhang Xichen, He Dengfa, Fan Rui, Wang Yanjun, Huang Linjun, Cui Jian, Liu Wenqiang, Yang Xiulei, 2023. Analogue Modeling of Structural Deformation of Tongnanba Anticline in Mesozoic and Cenozoic, NE Sichuan Basin. Earth Science, 48(4): 1307-1320. doi: 10.3799/dqkx.2022.423

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Analogue Modeling of Structural Deformation of Tongnanba Anticline in Mesozoic and Cenozoic, NE Sichuan Basin

doi: 10.3799/dqkx.2022.423

Ma Delong^{1, 2
,
,},
Wang Hongbin^{1, 2},
Zhang Xichen³,
He Dengfa⁴,
Fan Rui⁵,
Wang Yanjun^{1, 2},
Huang Linjun¹,
Cui Jian^{1, 2},
Liu Wenqiang²,
Yang Xiulei^{2, 6}

1.
Research Institute of Petroleum Exploration and Development-Northwest, PetroChina, Lanzhou 730020, China
2.
Key Laboratory of Reservoir Description, PetroChina, Lanzhou 730020, China
3.
Exploration Company, SINOPEC, Chengdu 610042, China
4.
School of Energy Resources, China University of Geosciences, Beijing 100083, China
5.
Research amd Development Center, BGP Inc., CNPC, Zhuozhou 072750, China
6.
School of Earth Sciences, East China University of Technology, Nanchang 330013, China

Received Date: 2022-06-12
Publish Date: 2023-04-25

Abstract

Abstract

Tongnanba anticline is located in the Northeast Sichuan basin, which is adjacent to the Micangshan Mountain to the north and Dabashan Mountain to the northeast. Conducting analogue modeling on tectonic relationships between Tongnanba anticline with surrounding mountains and paleo-uplift has important significance for constraining orogenic tectonic deformation time and sequences in the region, and also has importance significance for oil and gas exploration. In the model, shortening from north and northeast represents Micangshan Mountain and Dabashan Mountain, respectively. Lower silicone and upper sand are used to represent salts of Leikoupo Formation in Triassic and upper clastic rocks, respectively. The plasticene in the model acts as uplift developed in Paleozoic in NE Sichuan basin, which is widely accepted.Experiment results show that during compression from north moving wall, velocity vectors rapidly transferred to plasticene, which representing paleo-uplift, to form NE fold and thrust. During compression from northeast moving wall, NW trend arc-shape structures were formed imposing on the earlier formed NE trend structure. Combining with earlier reports on evolution histories, it makes conclusions that the evolution of Tongnanba anticline was controlled by surrounding Micang and Daba orogenic belts to form tectonic superposition of earlier NE trend structures and later NW trend structures. While, the Paleozoic NE trend uplift in NE Sichuan basin also controlled the orientation of Tongnanba anticline.
- NE Sichuan basin,
- Tongnanba anticline,
- uplift,
- analogue modeling,
- tectonic evolution,
- structural geology

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References(59)

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