东海盆地丽水凹陷T85构造变革界面的厘定及其成因模式探讨

蒋一鸣; 吴路路; 覃军; 唐贤君; 张彦振; 李泽宇; 沈传波

doi:10.3799/dqkx.2024.084

Volume 49 Issue 12

Dec. 2024

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Article Navigation > Earth Science > 2024 > 49(12): 4450-4464

Jiang Yiming, Wu Lulu, Qin Jun, Tang Xianjun, Zhang Yanzhen, Li Zheyu, Shen Chuanbo, 2024. Deciphering Tectonic Mechanism and Origin of T85 Horizon in Lishui Depression, East China Sea Basin. Earth Science, 49(12): 4450-4464. doi: 10.3799/dqkx.2024.084

Citation:

Jiang Yiming, Wu Lulu, Qin Jun, Tang Xianjun, Zhang Yanzhen, Li Zheyu, Shen Chuanbo, 2024. Deciphering Tectonic Mechanism and Origin of T85 Horizon in Lishui Depression, East China Sea Basin. Earth Science, 49(12): 4450-4464. doi: 10.3799/dqkx.2024.084

Citation:

Jiang Yiming, Wu Lulu, Qin Jun, Tang Xianjun, Zhang Yanzhen, Li Zheyu, Shen Chuanbo, 2024. Deciphering Tectonic Mechanism and Origin of T85 Horizon in Lishui Depression, East China Sea Basin. Earth Science, 49(12): 4450-4464. doi: 10.3799/dqkx.2024.084

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Deciphering Tectonic Mechanism and Origin of T85 Horizon in Lishui Depression, East China Sea Basin

doi: 10.3799/dqkx.2024.084

1.
Shanghai Branch of CNOOC Ltd., Shanghai 200335, China
2.
Key Laboratory of Tectonics and Petroleum Resources, Ministry of Education, China University of Geosciences, Wuhan 430074, China
3.
School of Energy Science and Engineering, Henan Polytechnic University, Jiaozuo 454003, China

Received Date: 2024-07-28
Available Online: 2025-01-09
Publish Date: 2024-12-25

Abstract

Abstract

To unravel the difference of rift evolution between the sub- and supra-T85 horizon, and illustrate the formation mechanism of the tectonic transition, the rift architecture, fault activity and spatio-temporal variations of subsidence were investigated by using high-quality seismic data and borehole data. Dividing by the T85 angular unconformity, the Lishui depression exhibits two distinct rift architecture: the underlying fault-controlled, wedge-shaped packages and the overlying saucer-shaped packages. Subsidence within the Lishui depression migrated westward during the faulting stage, while it progressively migrated eastward during the subsequent faulting and sagging stage. Together with the regional geodynamic context and advances in rift research, the study proposes that either the thermal subsidence caused by tectonic migration or the shallow response to the ductile deformation of lower crust resulted in the tectonic transition within the Lishui depression. The study significantly improves the understanding of rift evolution and its controlling factors.
- tectonic transition,
- rift evolution,
- unconformity,
- Lishui depression,
- East China Sea basin,
- petroleum geology

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References(58)

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Deciphering Tectonic Mechanism and Origin of T85 Horizon in Lishui Depression, East China Sea Basin

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