The Copper polymetallic deposits and resource potential in the Tibet Plateau

• DOI: 10.31035/cg2021016
• Publication Date: 2021-03-25T01:47:41Z
• Authors: Ju-xing Tang; ; Huan-huan Yang; Yang Song; Li-qiang Wang; Zhi-bo Liu; Bao-long Li; Bin Lin; Bo Peng; Gen-hou Wang; Qing-gao Zeng; Qin Wang; Wei Chen; Nan Wang; Zhi-jun Li; Yu-bin Li; Yan-bo Li; Hai-feng Li; Chuan-yang Lei
• Keywords: QE1-996.5; Geology; Resource potential; Mineral exploration engineering; Engineering (General). Civil engineering (General); 01 natural sciences; Tethys Ocean; Gangdese metallogenic belt; Porphyry-epithermal-skarn Cu deposit; Bangong Co-Nujiang metallogenic belt; TA1-2040; 0105 earth and related environmental sciences

ABSTRACT: Many large and super-large copper deposits have been discovered and explored in the Tibet Plateau, which makes it the most important copper resource reserve and development base in China. Based on the work of the research team, the paper summarizes the geological characteristics of the main copper deposits in Tibet and puts forward a further prospecting direction. A series of large accumulated metal deposits or ore districts from subduction of Tethys oceanic crust to India-Asia collisionhave been discovered, such as Duolong Cu (Au) ore district and Jiama copper polymetallic deposit. The ore deposits in the Duolong ore district are located in the lowstand domain, the top of lowstand domain, and the highstand domain of the same magmatic-hydrothermal metallogenic system, and their relative positions are the indicators for related deposits in the Bangong Co-Nujiang metallogenic belt. The polycentric metallogenic model of the Jiama copper polymetallic deposit is an important inspiration for the exploration of the porphyry mineralization related to collision orogeny. Further mineral exploration in the Tibet Plateau should be focused on the continental volcanic rocks related to porphyry-epithermal deposits, orogenic gold deposits, hydrothermal Pb-Zn deposits related to nappe structures, skarn Cu (Au) and polymetallic deposits, and the Miocene W-Sn polymetallic deposits.©2021 China Geology Editorial Office.