Sandbox modeling on the reworking of strike-slip faulting from pre-existing thrusts: A case study of Zhangjiakou-Penglai Fault Zone in Bohai area

LV Chunxiao; GUO Lingli; TAO Wei; ZHANG Jiaxuan; ZHOU Qijie; ZHANG Jingjing; CHEN Xin; WANG Guangzeng; LI Sanzhong

doi:10.16562/j.cnki.0256-1492.2023032802

Marine Geology & Quaternary Geology > 2024 > 44(4): 108-122. > DOI: 10.16562/j.cnki.0256-1492.2023032802

LV Chunxiao，GUO Lingli，TAO Wei，et al. Sandbox modeling on the reworking of strike-slip faulting from pre-existing thrusts: A case study of Zhangjiakou-Penglai Fault Zone in Bohai area[J]. Marine Geology & Quaternary Geology，2024，44(4)：108-122. DOI: 10.16562/j.cnki.0256-1492.2023032802

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Sandbox modeling on the reworking of strike-slip faulting from pre-existing thrusts: A case study of Zhangjiakou-Penglai Fault Zone in Bohai area

LV Chunxiao^{1, 2,},
GUO Lingli^{1, 2, ,},
TAO Wei^{1, 2},
ZHANG Jiaxuan^{1, 2},
ZHOU Qijie^{1, 2},
ZHANG Jingjing^{1, 2},
CHEN Xin^{1, 2},
WANG Guangzeng^{1, 2},
LI Sanzhong^{1, 2}

1.
Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Lab of Submarine Geosciences and Prospecting Techniques, MOE and College of Marine Geosciences, Ocean University of China, Qingdao 266100, China
2.
Laboratory for Marine Mineral Resources, Laoshan Laboratory, Qingdao 266237, China

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Received Date: March 27, 2023
Revised Date: May 20, 2023
Available Online: July 02, 2023

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Abstract

Abstract

It is common in nature for thrust structures to form new composite structural systems under the influence of strike-slip faulting. Since the Cenozoic, the sinistral strike-slip movement of the Zhangjiakou-Penglai fault zone in Bohai basin altered the pre-existed Yanshanian thrust structure. Driven by the subduction of the Pacific Plate since the Cenozoic, the NW-trending Zhangjiakou-Penglai fault zone fault zone co-worked with the conjugate NE-trending Tancheng-Lujiang fault zone and established the modern tectonic pattern of the Bohai Bay Basin. This area is an earthquake-prone area and also an oil-gas accumulation area. To understand the mechanism of strike-slip faulting from pre-existing thrusts, we conducted sandbox modeling with various strike-slip rates and basement rigidity setting. Results show a series of thrust faults forming thrust imbricate fan and pop-up structures under compression. After the superposition of thrusting by strike-slip motion, some strike-slip faults were formed and they cut through pre-existing thrusts, presenting a flower structure. Seen in the cross-section, the larger the strike-slip rate, the more faults, the larger the fault spacing, and the more complex flower structure. In the local plastic basement model, the strike-slip zone without superposition can form a fault depression. Combined with the tectonic evolution process of the study area, the modeled results showed a similar pattern of the tectonic pattern of the Zhangjiakou-Penglai fault zone, especially those of the flower structures in the Shabei fault and Shadong fault. Therefore, the strike-slip fault played a role in controlling the tectonic trap. This study provided a reference for understanding the dynamic mechanism of tectonic superposition of strike-slip faulting and thrusting.
- sandbox modeling,
- thrust-nappe structures,
- strike-slip structures,
- superimposed transformation,
- Zhangjiakou-Penglai fault zone

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References (78)

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