西藏拿若斑岩型铜(金)矿含矿岩体年代学、地球化学及地质意义

丁帅; 唐菊兴; 郑文宝; 杨超; 张志; 王勤; 王艺云

doi:10.3799/dqkx.2017.001

Volume 42 Issue 1

Jan. 2017

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Ding Shuai, Tang Juxing, Zheng Wenbao, Yang Chao, Zhang Zhi, Wang Qin, Wang Yiyun, 2017. Geochronology and Geochemistry of Naruo Porphyry Cu (Au) Deposit inDuolong Ore-Concentrated Area, Tibet, and Their Geological Significance. Earth Science, 42(1): 1-23. doi: 10.3799/dqkx.2017.001

Citation:

Ding Shuai, Tang Juxing, Zheng Wenbao, Yang Chao, Zhang Zhi, Wang Qin, Wang Yiyun, 2017. Geochronology and Geochemistry of Naruo Porphyry Cu (Au) Deposit in Duolong Ore-Concentrated Area, Tibet, and Their Geological Significance. Earth Science, 42(1): 1-23. doi: 10.3799/dqkx.2017.001

Citation:

Ding Shuai, Tang Juxing, Zheng Wenbao, Yang Chao, Zhang Zhi, Wang Qin, Wang Yiyun, 2017. Geochronology and Geochemistry of Naruo Porphyry Cu (Au) Deposit in Duolong Ore-Concentrated Area, Tibet, and Their Geological Significance. Earth Science, 42(1): 1-23. doi: 10.3799/dqkx.2017.001

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Geochronology and Geochemistry of Naruo Porphyry Cu (Au) Deposit in Duolong Ore-Concentrated Area, Tibet, and Their Geological Significance

doi: 10.3799/dqkx.2017.001

1.
College of Earth Science, Chengdu University of Technology, Chengdu 610059, China
2.
Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China
3.
Chengdu Center of China Geological Survey, Chengdu 610081, China

Received Date: 2016-07-15
Publish Date: 2017-01-15

Abstract

Abstract

As the most important part of Bangong Lake-Nujiang River metallogenic belt, the Duolong ore-concentrated area is characterized by the occurrence of huge mineralization scale, extended time span and complex forming process, resulting in controversial understanding of its petrogenesis and tectonics and those of related deposits. To address this problem, this study firstly presents new data of LA-ICP-MS zircon U-Pb age, whole-rock geochemistry, and in situ zircon Hf isotopes for the mineralization-associated granite porphyry in Naruo porphyry copper (gold) deposit, and secondly we make a detailed comparison with research results of other porphyry deposits in Duolong area to find out the tectonic setting, petrogenesis and geodynamic processes of the mineralization-associated porphyry in Duolong area. The test results show that the age of the Naruo Cu (Au) deposit formation is consistent with that of other deposits in Duolong area formed at Early Cretaceous about 120Ma. All the main intrusive rocks have similar lithogeochemical characteristics, for they all show the relative enrichment in light rare earth elements (LREE) and large-ion lithophile elements (LILE: Rb, Ba, K, etc.), relatively depleted in heavy rare earth elements (HREE ) and high field strength elements (HFSE: Nb, Ta, Zr, Hf, etc.). Moreover, the granite porphyry shows positive ε_Hf(t) values between 1.38-7.37, and two-stage model ages of zircons are 707-1086Ma. The results suggest that the formation of porphyry-epithermal copper (gold) deposit in Duolong ore-concentrated area is dominated by northward subduction of the Bangongcuo Tethys plate beneath Qiangtang block at Early Cretaceous. When the subducted oceanic crust reached 50-70km underground and generated different degrees of phase transformation, which leads to melt produced by dehydration of amphibole minerals metasomatized mantle wedge and induced mantle partial melting produced magmatic arc. Those deposits occurred in a continental arc tectonic setting which is similar to the continental margin arc environment of the ocean-continent subduction setting of the Andes metallogenic belt in South America.
- Naruo copper (gold) deposit,
- geochronology,
- geochemistry,
- Hf zircon isotope,
- continental arc,
- depleted mantle

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References(166)

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沈阳化工大学材料科学与工程学院沈阳 110142

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Geochronology and Geochemistry of Naruo Porphyry Cu (Au) Deposit in Duolong Ore-Concentrated Area, Tibet, and Their Geological Significance

doi: 10.3799/dqkx.2017.001

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