Pb同位素对努日铜钼钨多金属矿床成矿物源的制约

闫国强; 王欣欣; 黄勇; 李光明; 刘洪; 黄瀚霄; 张志; 田恩源; 赖杨

doi:10.3799/dqkx.2019.191

Volume 45 Issue 1

Jan. 2020

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Yan Guoqiang, Wang Xinxin, Huang Yong, Li Guangming, Liu Hong, Huang Hanxiao, Zhang Zhi, Tian Enyuan, Lai Yang, 2020. Constraint of Pb Isotope on Ore-Forming Source Origin of Nuri Polymetallic Deposit, Tibet. Earth Science, 45(1): 31-42. doi: 10.3799/dqkx.2019.191

Citation:

Yan Guoqiang, Wang Xinxin, Huang Yong, Li Guangming, Liu Hong, Huang Hanxiao, Zhang Zhi, Tian Enyuan, Lai Yang, 2020. Constraint of Pb Isotope on Ore-Forming Source Origin of Nuri Polymetallic Deposit, Tibet. Earth Science, 45(1): 31-42. doi: 10.3799/dqkx.2019.191

Citation:

Yan Guoqiang, Wang Xinxin, Huang Yong, Li Guangming, Liu Hong, Huang Hanxiao, Zhang Zhi, Tian Enyuan, Lai Yang, 2020. Constraint of Pb Isotope on Ore-Forming Source Origin of Nuri Polymetallic Deposit, Tibet. Earth Science, 45(1): 31-42. doi: 10.3799/dqkx.2019.191

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Constraint of Pb Isotope on Ore-Forming Source Origin of Nuri Polymetallic Deposit, Tibet

doi: 10.3799/dqkx.2019.191

Yan Guoqiang^{1,2
,
,},
Wang Xinxin^{3
,
,},
Huang Yong⁴,
Li Guangming⁴,
Liu Hong⁴,
Huang Hanxiao⁴,
Zhang Zhi⁴,
Tian Enyuan⁵,
Lai Yang⁵

1.
Tianjin Center, China Geological Survey, Tianjin 300170, China
2.
Key Laboratory of Uranium Geology, China Geological Survey, Tianjin 300170, China
3.
Institute of Coal Engineering, Shanxi Datong University, Datong 037003, China
4.
Chengdu Center, China Geological Survey, Chengdu 610081, China
5.
Institute of Mineral Resources Multi-Utilization, China Geological Survey, Chengdu 610061, China

Received Date: 2019-08-02
Publish Date: 2020-01-15

Abstract

Abstract

The Nuri Polymetallic Deposit,Tibet,is the largest and first scheelite deposit in Gangdese,and there have been some controversies on the ore-forming source of this deposit. The Pb isotope analyses of molybdenite,chalcopyrite,and pyrites from the mine have been carried out to determine the source. The results show that the molybdenite and pyrites have the consistent Pb isotopes,with ²⁰⁶Pb/²⁰⁴Pb ratios ranging from 17.525-18.581,²⁰⁷Pb/²⁰⁴Pb ratios ranging from 15.621-15.661,²⁰⁸Pb/²⁰⁴Pb ratios ranging from 37.524-38.929,and the chalcopyrite with ²⁰⁶Pb/²⁰⁴Pb ratios ranging from 18.414-18.578,²⁰⁷Pb/²⁰⁴Pb ratios ranging from 15.619-15.642,and ²⁰⁸Pb/²⁰⁴Pb ratios ranging from 38.617-38.863,respectively,which have obvious grouping characteristics. The S and Pb isotope features indicate that the ore-forming sources are mainly derived from the mantle,and the Re-Os isotope characteristics of molybdenite indicate that the minerals are mainly derived from mantle. The melt from the lower crust of India continent partial melting migrated upward and mixed with the Fe³⁺ enriched fluid derived from the subducted oceanic crust,which metasomatized with Yarlung Zangbo MORB peridotite,and the Cu,Mo were released into the magma system after oxidezed by Fe³⁺,thus,Cu and other elements in biotite granite which partially melted in the thickened lower crust were extracted in the rising process,finally formed the deposit by contact metasomatism with the wall rock.
- Nuri Polymetallic,
- Pb isotope,
- ore-forming source,
- Gangdese,
- adakite porphyry,
- geochemistry

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References(76)

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Constraint of Pb Isotope on Ore-Forming Source Origin of Nuri Polymetallic Deposit, Tibet

doi: 10.3799/dqkx.2019.191

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