YANSHANIAN STRUCTURAL DEFORMATION AND DYNAMICS OF THE XUEFENGSHAN INTRACONTINENTAL TECTONIC SYSTEM

LIU Enshan; LI Sanzhong; JIN Chong; DAI Liming; LIU Bo; ZHANG Guowei

doi:10.3724/SP.J.1140.2010.05063

2010 Vol. 30, No. 5

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Article navigation > Marine Geology & Quaternary Geology > 2010 > 30(5): 63-74

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LIU Enshan, LI Sanzhong, JIN Chong, DAI Liming, LIU Bo, ZHANG Guowei. YANSHANIAN STRUCTURAL DEFORMATION AND DYNAMICS OF THE XUEFENGSHAN INTRACONTINENTAL TECTONIC SYSTEM[J]. Marine Geology & Quaternary Geology, 2010, 30(5): 63-74. doi: 10.3724/SP.J.1140.2010.05063

Citation:

LIU Enshan, LI Sanzhong, JIN Chong, DAI Liming, LIU Bo, ZHANG Guowei. YANSHANIAN STRUCTURAL DEFORMATION AND DYNAMICS OF THE XUEFENGSHAN INTRACONTINENTAL TECTONIC SYSTEM[J]. Marine Geology & Quaternary Geology, 2010, 30(5): 63-74. doi: 10.3724/SP.J.1140.2010.05063

YANSHANIAN STRUCTURAL DEFORMATION AND DYNAMICS OF THE XUEFENGSHAN INTRACONTINENTAL TECTONIC SYSTEM

1 Key Lab of Submarine Geosciences and Prospecting Technique, Ministry of Education, Qindao 266100;
2 College of Marine Geoscience, Ocean University of China, Qindao 266100;
3 Northwest University, Xi'an 710069

Received Date: 19 February 2010

Revised Date: 07 July 2010

Abstract

Abstract

This paper deals with the geometry and temporal-spatial evolution of the Yanshanian faults and folds in the Xuefengshan intracontinental tectonic system. The results show that the structural pattern of the west of the Xuefengshan Mountain is obviously controlled by the blocking effect and the boundary faults between different structural units play a significant role in controlling structural styles. In general, there are two-stages of Yanshanian folding in this region. The early-stage fold extends in NE-NNE,and the late-stage fold in SN-NNE directions. Under the stress of SE-NW shortening, the Xuefengshan Precambrian basement lifted up vertically along some thrusts and escaped laterally along some strike-slip faults in a plane view. Separated by the Huaihua-Xinhuang fault, the south part of the Xuefengshan Precambrian basement escaped southwestward. Compared the subduction of the paleo-Pacific plate in the Yanshanian period with the Yanshanian deformation of the Xuefengshan intracontinental tectonic system, we can find that the northwestward and westward subduction of the paleo-Pacific plate possibly controlled the two stages of Yanshanian folding and thrusting in this region.
- Xuefengshan /
- intracontinental tectonics /
- escape tectonics /
- fold /
- South China

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References

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