Mesozoic multistage deformation and mechanism of the Central Bohai Bay Basin formation

LI Jinyue; HUANG Zhi; HU Zhiwei; ZHAO Shujuan; DAI Liming; YANG Yu; LI Fakun; ZHAN Huawang

doi:10.16562/j.cnki.0256-1492.2023112206

Marine Geology & Quaternary Geology > 2025 > 45(1): 154-167. > DOI: 10.16562/j.cnki.0256-1492.2023112206

LI Jinyue，HUANG Zhi，HU Zhiwei，et al. Mesozoic multistage deformation and mechanism of the Central Bohai Bay Basin formation[J]. Marine Geology & Quaternary Geology，2025，45(1)：154-167. DOI: 10.16562/j.cnki.0256-1492.2023112206

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Mesozoic multistage deformation and mechanism of the Central Bohai Bay Basin formation

LI Jinyue^{1, 2,},
HUANG Zhi³,
HU Zhiwei³,
ZHAO Shujuan^{1, 2, ,},
DAI Liming^{1, 2},
YANG Yu^{1, 2},
LI Fakun^{1, 2},
ZHAN Huawang^{1, 2}

1.
Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Lab of Submarine Geosciences and Prospecting Techniques, MOE, College of Marine Geosciences, Ocean University of China, Qingdao 266100, China
2.
Laboratory for Marine Mineral Resources, Qingdao Marine Science and Technology Center, Qingdao 266237, China
3.
Tianjin Branch of CNOOC(China)Limited, Tianjin 300452, China

More Information

Received Date: November 21, 2023
Revised Date: January 03, 2024
Accepted Date: January 03, 2024
Available Online: May 22, 2024

Graphical Abstract

Abstract

Abstract

Revealing the structural characteristics of multistage deformations and evolution of the Central Bohai Bay Basin during the Indosinian and Yanshanian could provide theoretical support for oil and gas exploration of buried-hills. Based on a detailed structural analysis on the 3D seismic data in the study area, we determined the stratigraphic division, tectonic sequence, and superimposed modification of late deformation on early one, and analyzed the mechanism of the deformation in each stage. The Central Bohai Bay Basin developed three main groups of faults in the Mesozoic. The Indosinian Movement triggered northward thrusting, forming NW to nearly EW-trending imbricated thrust faults that underwent negative inversion during the Late Jurassic to Early Cretaceous. The NNE to nearly SN-trending tear faults formed during the Indosinian regulated the movement among different blocks. The Yanshanian Movement evidenced two episodes of NW-SE compression during the late Middle Jurassic and Late Cretaceous, respectively. The compression formed NE-SW-trending reverse faults of which some parts inherited Indosinian fault plane. In addition, the Indosinian tear faults evolved into transpressional sinistral strike-slip faults in the Yanshanian, constraining the scale of the NE-trending reverse faults.
- superimposed modification,
- Mesozoic,
- Indosinian,
- Yanshanian,
- Bohai Bay Basin

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References (55)

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