GEOLOGICAL STRUCTURE CHARACTERISTICS OF THE NORTHERN SEGMENT OF XUEFENG OROGEN: A CASE STUDY OF THE CILI-ANHUAN CORRIDOR

BAI Dao-yuan; ZHONG Xiang; JIA Peng-yuan; WANG Xian-hui; PENG Yun-yi

Volume 21 Issue 3

Sep. 2015

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Article Navigation > Journal of Geomechanics > 2015 > 21(3): 399-414

BAI Dao-yuan, ZHONG Xiang, JIA Peng-yuan, et al., 2015. GEOLOGICAL STRUCTURE CHARACTERISTICS OF THE NORTHERN SEGMENT OF XUEFENG OROGEN: A CASE STUDY OF THE CILI-ANHUAN CORRIDOR. Journal of Geomechanics, 21 (3): 399-414.

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GEOLOGICAL STRUCTURE CHARACTERISTICS OF THE NORTHERN SEGMENT OF XUEFENG OROGEN: A CASE STUDY OF THE CILI-ANHUAN CORRIDOR

Hunan Institute of Geology Survey, Changsha, 410016, China

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Received: 2015-03-10
Published: 2015-09-01

Abstract

Abstract

Cili-Anhuan corridor was taken as examples for studying the geological structure characteristics of the western part of the northern Xuefeng orogen. It is shown that the northern segment of Xuefeng orogen is composed of the northern Wuling fault-bend fold belt and the southern Xuefeng basement detachment belt. There existed main deformation types such as NEE-EW trending folds and thrust faults in the Wuling fault-bend fold belt with minor NE-NNW trending dextral strike-slip faults and NEE-EW trending normal faults. And there existed EW-NE trending folds, EW-NE trending thrust faults and normal faults with minor NE trending strike-slip faults in the Xuefeng basement detachment belt. The deformations in the Wuling fault-bend fold belt were controlled mainly by the northward detachment of the bottom of the Banxi Group and thrust faults. While the deformations in the Xuefeng basement detachment belt were controlled mainly by the detachment and thrust faults cutting through the Lengjiaxi Group fold-basement, with the direction from north to south in overall and then turning to south at the southern margin. The folds and faults in the northern segment of Xuefeng orogen were formed in the compression events of Wuling Movement, Caledonian Movement, Indosinian Movement and Early Yanshanian Movement, following by the extension in Cretaceous, the NE-NNE direction regional compression during middle-late Paleogene and the NW direction compression during late Paleogene-early Neogene. Among which the folds and thrust faults formed in the Caledonian Movement and Indosinian Movement are the most important. There existed back-thrust structures both in the northern segment and the middle-southern segment of Xuefeng orogen, however there existed stronger thrusting, thickening and uplift in the northern segment controlled by the Caledonian regional S-N compression.
- northern segment of the Xuefeng orogen,
- Cili-Anhuan corridor,
- fold,
- fault,
- Caledonian Movement,
- Indosinian Momement,
- back thrust structures

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