西藏冈底斯成矿带南缘新特提斯洋俯冲期成矿作用: 来自雄村矿集区Ⅰ号矿体的Re-Os同位素年龄证据

郎兴海; 唐菊兴; 陈毓川; 李志军; 黄勇; 王成辉; 陈渊; 张丽; 周云

doi:10.3799/dqkx.2012.058

Volume 37 Issue 3

May 2012

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Article Navigation > Earth Science > 2012 > 37(3): 515-525

LANG Xing-hai, TANG Ju-xing, CHEN Yu-chuan, LI Zhi-jun, HUANG Yong, WANG Cheng-hui, CHEN Yuan, ZHANG Li, ZHOU Yun, 2012. Neo-Tethys Mineralization on the Southern Margin of the Gangdise Metallogenic Belt, Tibet, China: Evidence from Re-Os Ages of Xiongcun Orebody No. Ⅰ. Earth Science, 37(3): 515-525. doi: 10.3799/dqkx.2012.058

Citation:

LANG Xing-hai, TANG Ju-xing, CHEN Yu-chuan, LI Zhi-jun, HUANG Yong, WANG Cheng-hui, CHEN Yuan, ZHANG Li, ZHOU Yun, 2012. Neo-Tethys Mineralization on the Southern Margin of the Gangdise Metallogenic Belt, Tibet, China: Evidence from Re-Os Ages of Xiongcun Orebody No. Ⅰ. Earth Science, 37(3): 515-525. doi: 10.3799/dqkx.2012.058

Citation:

LANG Xing-hai, TANG Ju-xing, CHEN Yu-chuan, LI Zhi-jun, HUANG Yong, WANG Cheng-hui, CHEN Yuan, ZHANG Li, ZHOU Yun, 2012. Neo-Tethys Mineralization on the Southern Margin of the Gangdise Metallogenic Belt, Tibet, China: Evidence from Re-Os Ages of Xiongcun Orebody No. Ⅰ. Earth Science, 37(3): 515-525. doi: 10.3799/dqkx.2012.058

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Neo-Tethys Mineralization on the Southern Margin of the Gangdise Metallogenic Belt, Tibet, China: Evidence from Re-Os Ages of Xiongcun Orebody No. Ⅰ

doi: 10.3799/dqkx.2012.058

1.
College of Earth Sciences, Chengdu University of Technology, Chengdu 610059, China
2.
Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China
3.
Xizang (Tibet) Tianyuan Minerals Exploration Ltd., Shigatse 857000, China
4.
Chengdu Center of China Geological Survey, Chengdu 610081, China

Received Date: 2011-04-02
Available Online: 2021-11-09
Publish Date: 2012-05-01

Abstract

Abstract

Xiongcun metallogenic district, one of the large-size metallogenic areas discovered along Gangdise metallogenic belt, is located in the middle of the southern margin of Gangdise orogenic belt. Its south margin is Shigatse forearc basin. The latest exploration data indicate that Xiongcun metallogenic district is composed of No. Ⅰ, Ⅱ and Ⅲ porphyry copper-gold orebodies. In this paper, Xiongcun orebody No.Ⅰ is taken as the research subject. The Re-Os model ages of molybdenit (4 samples) from Xiongcun orebody No.Ⅰ are similar, ranging from 160.1±2.3 Ma to 163.4±2.3 Ma; its isochron age is 161±11 Ma (MSWD=4.2) and error is big; its weight average age is 161.5±2.7 Ma (MSWD=2.0) and error is small. So ore forming age of Xiongcun orebody No. Ⅰ is (160.1±2.3)-(163.4±2.3) Ma and the most probability is 161.5±2.7 Ma. This age is similar to zircon U-Pb age (164.3±1.9 Ma) of mineralization porphyry (hornblende quartz diorite porphyry with big quartz eyes), so the ore forming age of Xiongcun orebody No.Ⅰ is Middle Jurassic. In addition, mineralized porphyry and tuff show geochemical characteristics similar to those of volcanic rocks in an arc or active continental margin, such as relative enrichment of LREE and LILE, depletion of HFEE, HFS and Eu anomalies. We conclude that northward subduction of Neo-Tethys resulted in mineralization of the Xiongcun orebody No.Ⅰ in the Middle Jurassic; the tectonic setting is the island-arc environment. The deposit type of Xiongcun orebody No.Ⅰ is island arc type porphyry copper-gold deposit.
- Re-Os dating,
- molybdenite,
- porphyry,
- mineralization,
- Tibet,
- Neo-Tethys Ocean

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Neo-Tethys Mineralization on the Southern Margin of the Gangdise Metallogenic Belt, Tibet, China: Evidence from Re-Os Ages of Xiongcun Orebody No. Ⅰ

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