黄海及邻区晚中生代构造转换与原型盆地构造格局

周瑶琪; 张悦; 周腾飞; 商跃瀚; 李孙义; 白冰洋; 陈扬; 穆宏玉

doi:10.3799/dqkx.2022.174

Volume 48 Issue 4

Apr. 2023

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Article Navigation > Earth Science > 2023 > 48(4): 1461-1480

Zhou Yaoqi, Zhang Yue, Zhou Tengfei, Shang Yuehan, Li Sunyi, Bai Bingyang, Chen Yang, Mu Hongyu, 2023. Tectonic Transition of the Late-Mesozoic Yellow Sea and Adjacent Region and Its Tectonic Framework of the Proto-Basin. Earth Science, 48(4): 1461-1480. doi: 10.3799/dqkx.2022.174

Citation:

Zhou Yaoqi, Zhang Yue, Zhou Tengfei, Shang Yuehan, Li Sunyi, Bai Bingyang, Chen Yang, Mu Hongyu, 2023. Tectonic Transition of the Late-Mesozoic Yellow Sea and Adjacent Region and Its Tectonic Framework of the Proto-Basin. Earth Science, 48(4): 1461-1480. doi: 10.3799/dqkx.2022.174

Citation:

Zhou Yaoqi, Zhang Yue, Zhou Tengfei, Shang Yuehan, Li Sunyi, Bai Bingyang, Chen Yang, Mu Hongyu, 2023. Tectonic Transition of the Late-Mesozoic Yellow Sea and Adjacent Region and Its Tectonic Framework of the Proto-Basin. Earth Science, 48(4): 1461-1480. doi: 10.3799/dqkx.2022.174

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Tectonic Transition of the Late-Mesozoic Yellow Sea and Adjacent Region and Its Tectonic Framework of the Proto-Basin

doi: 10.3799/dqkx.2022.174

1.
School of Geoscience and Technology, China University of Petroleum, Qingdao 266580, China
2.
Exploration and Development Research Institute, Shengli Oilfield Company, SINOPEC, Dongying 257015, China

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

Abstract

Abstract

The subduction, rollbacking and the direction of the subduction of the Paleo-Pacific Plate had a significant influence on the development of the basins in the Yellow Sea and its adjacent areas. According to the drilling core data of the field profile and marine seismic profile, the sedimentation between different basins is compared and analyzed, and the changes of the stress field direction and main tectonic deformation framework in different periods are identified. Meanwhile, the main faults are defined, critical time nodes have provided evidence, and the research area's tectonic transition from the Jurassic to the Cretaceous is restored. The results indicate that: (1) Under the background of the subduction of the paleo-pacific plate, the basin has undergone multiple stages of 'extension' and 'compression' structural stress fields and under the joint control of the two main fault zones of the Tanlu fault zone F1 and the western Korean Peninsula fault zone F2. (2) During Laiyang period, passive rift was developed due to the stretching from south to north; At 125±1 Ma stage, thermal uplift extrusion caused slight tectonic inversion and formed angular unconformity in the uplift area; The volcanic arc basin with active rift was formed during the Qingshan period; At the extrusion stage of 87.5±2.5 Ma, large-scale sinistral strike-slip occurred and regional angular unconformity was formed; The thermal subsidence in Wang stage formed a large area depression with the nature of take-away slip and pull-apart; At the extrusion stage of 50±5 Ma, dextral strike-slip occurred mainly at F1 and F2 faults. (3) In this paper, the strike-slip amount in the extrusion stage is estimated, and the elongation and settlement rate in the extension stage are calculated. It is the first time to reconstruct the tectonic framework and basin prototype before the evolution of the Late Mesozoic compressive tectonic episode in the Yellow Sea and adjacent areas of China, and to explain the influence of the subduction of the Paleo-Pacific plate on the evolution of the tectonic framework in the Yellow Sea and adjacent areas.
- Mesozoic Era,
- Layang period,
- Qingshan period,
- Wang period,
- rift basin,
- Paleo-Pacific Plate subduction,
- The Chinese Yellow Sea,
- structural geology

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References(86)

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Tectonic Transition of the Late-Mesozoic Yellow Sea and Adjacent Region and Its Tectonic Framework of the Proto-Basin

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