The division of mélanges in the orogenic belt and its associated terminologies

ZHANG Kexin; LI Yangchun; WANG Lijun; WANG Jiaxuan; XU Yadong; WANG Yonghe; XIN Houtian; ZHAO Xiaoming; YIN Fuguang; LI Zhipei; GU Yongchang; YANG Zhuliang; FU Junyu

2020 Vol. 39, No. 6

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ZHANG Kexin, LI Yangchun, WANG Lijun, WANG Jiaxuan, XU Yadong, WANG Yonghe, XIN Houtian, ZHAO Xiaoming, YIN Fuguang, LI Zhipei, GU Yongchang, YANG Zhuliang, FU Junyu. The division of mélanges in the orogenic belt and its associated terminologies[J]. Geological Bulletin of China, 2020, 39(6): 765-782.

Citation:

ZHANG Kexin, LI Yangchun, WANG Lijun, WANG Jiaxuan, XU Yadong, WANG Yonghe, XIN Houtian, ZHAO Xiaoming, YIN Fuguang, LI Zhipei, GU Yongchang, YANG Zhuliang, FU Junyu. The division of mélanges in the orogenic belt and its associated terminologies[J]. Geological Bulletin of China, 2020, 39(6): 765-782.

The division of mélanges in the orogenic belt and its associated terminologies

1.
Institute of Geological Survey, China University of Geosciences, Wuhan 430074, Hubei, China
2.
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, Hubei, China
3.
Development and Research Center of China Geological Survey, Beijing 100037, China
4.
Xi'an Center of Geological Survey, CGS, Xi'an 710054, Shaanxi, China
5.
Tianjin Center of Geological Survey, CGS, Tianjin 710054, China
6.
Wuhan Center of Geological Survey, CGS, Wuhan 430223, Hubei, China
7.
Chengdu Center of Geological Survey, CGS, Chengdu 610082, Sichuan, China
8.
Nanjing Center of Geological Survey, CGS, Nanjing 210016, Jiangsu, China
9.
Shenyang Center of Geological Survey, CGS, Shenyang 110032, Liaoning, China

Received Date: 15 October 2019

Revised Date: 22 February 2020

Publish Date: 15 June 2020

Abstract

Abstract

The area of orogenic belts in China covers nearly three-fifths of the land area.Multiple episodes of deformation during the tectonic evolution of orogenic belts, such as archipelagic ocean evolution, continental subduction-accretion and continental collision, caused diverse types of mélanges.Therefore, it is the key point and challenges to differentiate various types of mélanges and recognize the primary block-in-matrix fabric of the mélange on the basis of geological mapping.In this paper, the authors have made a brief introduction and exposition of the current concepts of mélange and mélange nomenclature, such as ophiolite, ophiolite mélange, subduction-accreation complex, complex, slice, superslice, non-Smith strata, tectonostratigraphy, ocean plate stratigraphy, subordinate suture zone and main suture zone.The authors divide the mélanges into three types:olistostrome(sedimentary mélange), tectonic mélange, and sedimentary-tectonic polygenetic mélange, based on the features of orogenic belts in China.Olistostrome(sedimentary mélange)was formed in an extensional environment during the early stage of the Wilson cycle.The other two were formed at the late stage in association with the evolution of oceanic crust subduction or continental collision.Subduction-accretion complex is the product of tectonic mélange as a result of subduction-accretion process in the subduction zone.
- mélange /
- subduction-accretion complex /
- tectonic mélange /
- orogenic belt /
- China

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References

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