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LIU Shusheng, YANG Yongfei, GUO Linnan, NIE Fei, PENG Zhiming, PAN Guitang. 2018. Tectonic characteristics and metallogeny in Southeast Asia[J]. Geology in China, 45(5): 863-889. doi: 10.12029/gc20180501
Citation: LIU Shusheng, YANG Yongfei, GUO Linnan, NIE Fei, PENG Zhiming, PAN Guitang. 2018. Tectonic characteristics and metallogeny in Southeast Asia[J]. Geology in China, 45(5): 863-889. doi: 10.12029/gc20180501
shu

Tectonic characteristics and metallogeny in Southeast Asia

  • 1.

    College of Earth Sciences, Chengdu University Of Technology, Chengdu 610059, Sichuan, China

  • 2.

    Chengdu Center, China Geological Survey, Chengdu 610081, Sichuan, China

    • Fund Project: Supported by China Geological Survey Program (No. DD20160107) and National Natural Science Foundation of China (No. 41702087)
More Information
  • Author Bio: LIU Shusheng, male, born in 1977, senior engineer, majors in evaluation of mineral resources potential in Southeast Asia and South Asia; E-mail: cdlshusheng@qq.com.
  • Corresponding author: YANG Yongfei, male, born in 1984, doctor, majors in tectonics and metallogenesis in Southeast Asia; E-mail:yyf6811@163.com. 
Received Date:  03 September 2018
Revised Date:  28 September 2018
Publish Date:  25 October 2018
    Abstract

  • Southeast Asia is located at the intersection of the Tethys, the circum-Pacific and the India-Australia metallogenic domain. The tectonic evolution is unique in that it has experienced multi-stage tectonic-magmatic events including the Proto-, Paleo-, Meso-, and Neo-Tethys accreting orogenesis, collisional orogenesis between the Indian Plate and Eurasian Plate, and the Pacific plate subduction. These activities have developed many volcanic arcs, ophiolite belts, and post-collision magmatic belts in Southeast Asia. Based on the previous tectonic researches, this paper divides Southeast Asia into 6 first-order, 32 second-order and 57 third-order tectonic units. Along with the multi-stage tectonic events including evolution of the Proto-, Paleo-, Meso-, and Neo-Tethys, the Indian-Eurasian collision, and the Pacific subduction and on the basis of the tectonic-unit division, this paper divides the Southeast Asian region into 3 first-level metallogenic domains, 6 second-level metallogenic provinces, and 21 thirdlevel metallogenic belts. The main metallogenic events are discussed in combination with tectonic evolution.

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