Structural Features and Evolutionary History of  Qiaojia Pull-Apart Basin

PEI Xiangjun; LI Tiantao; HUANG Runqiu; WANG Shuang

doi:10.3969/j.issn.0258-2724.20170206

Volume 54 Issue 2

Jun. 2019

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Journal of Southwest Jiaotong University > 2019 > 54(2): 278-286.

PEI Xiangjun, LI Tiantao, HUANG Runqiu, WANG Shuang. Structural Features and Evolutionary History of Qiaojia Pull-Apart Basin[J]. Journal of Southwest Jiaotong University, 2019, 54(2): 278-286. doi: 10.3969/j.issn.0258-2724.20170206

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PEI Xiangjun, LI Tiantao, HUANG Runqiu, WANG Shuang. Structural Features and Evolutionary History of Qiaojia Pull-Apart Basin[J]. Journal of Southwest Jiaotong University, 2019, 54(2): 278-286. doi: 10.3969/j.issn.0258-2724.20170206

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Structural Features and Evolutionary History of Qiaojia Pull-Apart Basin

doi: 10.3969/j.issn.0258-2724.20170206

Received Date: 22 Mar 2017
Rev Recd Date: 24 Jul 2017

Available Online: 27 Sep 2017

Publish Date: 01 Apr 2019

Abstract

Abstract

In order to explore the features, formation and evolution process of the Qiaojia Basin, detailed field investigation was carried out. Firstly, based on the investigation, the basic geological background conditions of the study area and the sedimentary characteristics of the basin surface were mastered. Further, the borehole survey was carried out on the central area of the basin, and the internal structural characteristics of the basin were obtained. Combing with the regional geological background and the structural characteristics, the formation and evolution process of the basin was analyzed. The results show that the Qiaojia Basin is a typical pull-apart basin, which is mainly controlled by the Xiaojiang Fault. The internal structure of the basin mainly includes five stratigraphic sequences: the alluvial layer of the ancient river, the hydrostatic sedimentary layers, the debris flow alluvium, and the river terraces. It is first discovered that a large-scale damming event occurred 3 km from the downstream boundary of the basin about 30 000 years ago. It is presumed that the basin formed during the late Tertiary period, and later experienced the effects of pull-apart process, damming process, debris flow events, and alluvial events. Through rigorous analysis and research, the evolution process of the basin was divided into 6 stages: regional dislocation, local pull-apart rifting, rift lake deposition, barrier lake deposition, barrier lake breaking, and uneven lifting.
- Xiaojiang Fault,
- pull-apart basin,
- ancient landslide,
- barrier dam,
- evolutionary history

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Structural Features and Evolutionary History of Qiaojia Pull-Apart Basin

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