Evolution and Coal-forming Environment Analysis of Jurassic Rift Basin in Kusilafu Area, Western Kunlun

HUANG Jianguo; CUI Chunlong; YANG Jian; LI Wenjie; HOU Lanjie

Northwestern Geology > 2016 > 49(4): 201-206.

HUANG Jianguo, CUI Chunlong, YANG Jian, et al. Evolution and Coal-forming Environment Analysis of Jurassic Rift Basin in Kusilafu Area, Western Kunlun[J]. Northwestern Geology, 2016, 49(4): 201-206.

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Evolution and Coal-forming Environment Analysis of Jurassic Rift Basin in Kusilafu Area, Western Kunlun

College of Environment and Resources, Southwest University of Science and Technology, Mianyang 621010, Sichuan, China

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Received Date: November 24, 2015
Revised Date: June 17, 2016
Available Online: July 28, 2022
Published Date: December 04, 2016

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Abstract

Abstract

Rift basin is expanded with nearly N-S trending in Kusilafu area of Western Kunlun, which is controlled by regional Kusilafu Fault in the west. The coal of this rift basin is mainly produced in Yangye Formation and Shalitashi Formation of Jurassic Yeerqiang Group, showing the characteristics of multiple layers, thin layer and unstable elongation. Freshwater shelly beach and petrified wood stacked layers are also appeared in multiple layers, which show accumulation characteristics of coal plant's different burial places. Coal-forming environment belongs to thecontinental sedimentary environment of lacustrine and fluvial swamp. The stretching tectonic activity in Late Indo-China orogeny may be offer the impetus for the forming of coal-bearing rift basin nearby Kusilafu area.
- Western Kunlun,
- Kusilafu,
- Jurassic,
- rift basin,
- coal-forming environment

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Evolution and Coal-forming Environment Analysis of Jurassic Rift Basin in Kusilafu Area, Western Kunlun

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