Structural Characteristics and Plate Boundary Properties of the Kangguertage Fault Zone in Jueluotage Orogenic Belt, Eastern Tianshan

CAO Rui; MUHETAER Zari; WANG Dunke; CAO Fugen

Northwestern Geology > 2016 > 49(3): 28-38.

CAO Rui, MUHETAER Zari, WANG Dunke, et al. Structural Characteristics and Plate Boundary Properties of the Kangguertage Fault Zone in Jueluotage Orogenic Belt, Eastern Tianshan[J]. Northwestern Geology, 2016, 49(3): 28-38.

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Structural Characteristics and Plate Boundary Properties of the Kangguertage Fault Zone in Jueluotage Orogenic Belt, Eastern Tianshan

1. College of Earth Sciences, Chengdu University of Technology, Chengdu 610059, Sichuan, China;
2. Key Laboratory of Tectonic Controls on Mineralization and Hydrocarbon Accumulation, Ministry of Land and Resources, Chengdu University of Technology, Chengdu 610059, Sichuan, China;
3. Xinjiang Key Laboratory for Geodynamic Processes and Metallogenic Prognosis of Central Asian Orogenic Belt, Urumqi 830046, Xinjiang, China;
4. College of Geology and Mining Engineering, Xinjiang University, Urumqi 830046, Xinjiang, China;
5. No. 1 Brigade of Regional Geological Survey, Geological Bureau of Xinjiang, Urumqi 830046, Xinjiang, China

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Received Date: February 01, 2016
Revised Date: April 24, 2016
Available Online: July 28, 2022
Published Date: September 04, 2016

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Abstract

Abstract

Served as an important part of Central Asian orogenic belt, the Jueluotage area is the key collision belt between Tarim plate and Paleo-Asian Ocean. However, its tectonic attribution has been controversial. The Kangguertage fault zone is the boundary fault of the Jueluotageorogenic belt, the study of structure characteristics has important enlightenment function on the tectonic evolution about this area. In this paper, the Kangguertage fault zone has been studied ongeological characteristics, volcanic sediment and evolution. The results show that the Kangguertage zone is a ductile shear belt in deep leveland is characterized by apparent strike-slip; The carboniferous volcanic rocks in this area show typical characteristics of trench-arc-basin volcano-sedimentary formations; The area between Kangguertage and Aqqikkuduk fault zones is the collision suture belt of Junggar and Tarim Plates; From Late Carboniferous to Early Permian, the asymmetric bisubduction took place southward and northward in Kangguer Ocean respectively, causing the formation of Kangguertage-Aqqikkuduk suture zone, with the Kangguertage fault zone served as a northern border of this suture zone.
- Jueluotage orogenic belt,
- Kangguertage fault zone,
- tectonic feature,
- fault properties

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Structural Characteristics and Plate Boundary Properties of the Kangguertage Fault Zone in Jueluotage Orogenic Belt, Eastern Tianshan

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