西藏冈底斯成矿带西段矿床类型、成矿作用和找矿方向

黄瀚霄; 张林奎; 刘洪; 李光明; 黄勇; 兰双双; 吕梦鸿

doi:10.3799/dqkx.2018.364

Volume 44 Issue 6

Jun. 2019

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Article Navigation > Earth Science > 2019 > 44(6): 1876-1887

Huang Hanxiao, Zhang Linkui, Liu Hong, Li Guangming, Huang Yong, Lan Shuangshuang, Lü Menghong, 2019. Major Types, Mineralization and Potential Prospecting Areas in Western Section of the Gangdise Metallogenic Belt, Tibet. Earth Science, 44(6): 1876-1887. doi: 10.3799/dqkx.2018.364

Citation:

Huang Hanxiao, Zhang Linkui, Liu Hong, Li Guangming, Huang Yong, Lan Shuangshuang, Lü Menghong, 2019. Major Types, Mineralization and Potential Prospecting Areas in Western Section of the Gangdise Metallogenic Belt, Tibet. Earth Science, 44(6): 1876-1887. doi: 10.3799/dqkx.2018.364

Citation:

Huang Hanxiao, Zhang Linkui, Liu Hong, Li Guangming, Huang Yong, Lan Shuangshuang, Lü Menghong, 2019. Major Types, Mineralization and Potential Prospecting Areas in Western Section of the Gangdise Metallogenic Belt, Tibet. Earth Science, 44(6): 1876-1887. doi: 10.3799/dqkx.2018.364

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Major Types, Mineralization and Potential Prospecting Areas in Western Section of the Gangdise Metallogenic Belt, Tibet

doi: 10.3799/dqkx.2018.364

1.
Chengdu Center, China Geological Survey, Chengdu 610081, China
2.
Sichuan Institute of Metallurgical Geology and Exploration, Chengdu 610051, China

Received Date: 2018-08-17
Publish Date: 2019-06-15

Abstract

Abstract

Based on previous findings, in this study we conducted field and indoor investigations. We discusses deposit types, spatial and temporal distribution and associated characteristics, metallogenesis, and future prospecting direction of the metallic ore deposits in western Gangdese metallogenic belt (GMB). The results indicate that the metallic ore deposits (or ore spots) in the GMB are composed mainly of skarn-, porphyry-and epithermal-type deposits. These deposits spatially occur along a W-E trending belt and formed within Mesozoic and Cenozoic. The GMB can be divided into five critical periods according to deposit genesis and dynamic settings, including:(1) copper-gold polymetallic mineralization during Late Triassic to Late Cretaceous associated with Neo-Tethys northward subduction; (2) iron-copper-gold polymetallic mineralization during Middle Jurassic to Early Cretaceous associated with Middle-Tethys southward subduction; (3) copper-gold-molybdenum polymetallic mineralization during early of Late Cretaceous to Late Cretaceous associated with collision between Qiangtang and Lhasa blocks; (4) copper-lead-zinc-silver polymetallic mineralization during late of Late Cretaceous to Eocene associated with collision between Asian and Indian continents; and (5) copper-gold-molybdenum polymetallic mineralization during Miocene associated with extension following collision between Asian and Indian continents. Prominent minerals in the GMB are copper, iron, lead-zinc, gold-silver, etc.
- Gangdise metallogenic belt,
- deposit type,
- metallogenic regularity,
- mineralization,
- prospecting direction,
- geochemistry

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