南黄海盆地中部隆起构造特征及其成因机制

张田; 朱伟林; 胡森清; 陈春峰; 高顺莉; 陈忠云; 付晓伟; 钟锴

doi:10.3799/dqkx.2020.380

Volume 46 Issue 10

Nov. 2021

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Article Navigation > Earth Science > 2021 > 46(10): 3481-3495

Zhang Tian, Zhu Weilin, Hu Senqing, Chen Chunfeng, Gao Shunli, Chen Zhongyun, Fu Xiaowei, Zhong Kai, 2021. Structural Characteristic and Its Genetic Mechanism of Central Uplift in South Yellow Sea Basin. Earth Science, 46(10): 3481-3495. doi: 10.3799/dqkx.2020.380

Citation:

Zhang Tian, Zhu Weilin, Hu Senqing, Chen Chunfeng, Gao Shunli, Chen Zhongyun, Fu Xiaowei, Zhong Kai, 2021. Structural Characteristic and Its Genetic Mechanism of Central Uplift in South Yellow Sea Basin. Earth Science, 46(10): 3481-3495. doi: 10.3799/dqkx.2020.380

Citation:

Zhang Tian, Zhu Weilin, Hu Senqing, Chen Chunfeng, Gao Shunli, Chen Zhongyun, Fu Xiaowei, Zhong Kai, 2021. Structural Characteristic and Its Genetic Mechanism of Central Uplift in South Yellow Sea Basin. Earth Science, 46(10): 3481-3495. doi: 10.3799/dqkx.2020.380

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Structural Characteristic and Its Genetic Mechanism of Central Uplift in South Yellow Sea Basin

doi: 10.3799/dqkx.2020.380

Zhang Tian^{1, 2
,
,},
Zhu Weilin^{1, 2},
Hu Senqing³,
Chen Chunfeng³,
Gao Shunli³,
Chen Zhongyun³,
Fu Xiaowei^{1, 2},
Zhong Kai^{1, 2}

1.
State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China
2.
Center for Marine Resources, Tongji University, Shanghai 200092, China
3.
Shanghai Branch of CNOOC (China) Ltd., Shanghai 200335, China

Received Date: 2020-06-09
Available Online: 2021-11-03
Publish Date: 2021-11-03

Abstract

Abstract

By selecting typical seismic sections with clear internal seismic reflection and obvious structural features to carry out delicate structural interpretation, in this paper it systematically combines the structural style features of the central uplift in the South Yellow Sea basin, and identified the compressional structures (detachment, high angle thrust, opposite/back thrust), strike slip faults (positive flower, y-shaped), extensional normal fault (shovel-like normal fault) in the central uplift of the South Yellow Sea basin and so on. Among them, two NW-SE strike slip faults are proposed for the first time. On this basis, combined with the characteristics of regional stress field and the background of deep geodynamics, the development period, genetic mechanism and structural evolution course of the structural style in the central uplift are defined. The results show follows. (1) The detachment structure was mainly located in the north of the central uplift, and the detachment surface was located in the shale at the bottom of the Silurian strata. The tectonic stress mechanism of detachment originated from the collision orogeny between the North China plate and the Lower Yangtze plate at the end of Triassic. (2) The high angle thrust was mainly located in the south of the central uplift. The stress mechanism of the high angle thrust came from the initial high-speed and low angle NW subduction of the ancient Pacific plate during the early Yanshanian movement in Early Jurassic. (3) The strike slip faults were mainly positive flower structures with compression and torsion characteristics, which were located in the southeast and mid-west of the central uplift. The stress mechanism came from the sinistral shear caused by the low angle subduction of the ancient Pacific plate from NW to NNW in Early Cretaceous. The Tan-Lu fault in eastern China also showed sinistral shear characteristics in this period. (4) The extensional normal fault was characterized by shovel-like normal fault, which was developed in the north-south boundary of the central uplift, that was, the contact parts between the central uplift and the southern depression, the northern depression of the South Yellow Sea basin. The stress mechanism was derived from the transition of the paleo Pacific plate from low angle subduction to high angle subduction during the late Yanshanian movement in Late Cretaceous. At this time, the tectonic stress system in eastern China also changed from compression to extension.
- tectonic evolution,
- genetic mechanism,
- structural style,
- Mesozoic-Paleozoic,
- central uplift,
- South Yellow Sea basin,
- structural geology

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References(73)

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Structural Characteristic and Its Genetic Mechanism of Central Uplift in South Yellow Sea Basin

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