东昆仑浪木日铜多金属矿床成矿特征及找矿启示

童海奎; 龙灵利; 王玉往; 祝新友; 李顺庭; 谷子成; 马财; 代岩; 李杰; 于小亮; 王成勇; 王新雨; 张志超

doi:10.3799/dqkx.2023.028

Volume 48 Issue 12

Dec. 2023

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Article Navigation > Earth Science > 2023 > 48(12): 4349-4369

Tong Haikui, Long Lingli, Wang Yuwang, Zhu Xinyou, Li Shunting, Gu Zicheng, Ma Cai, Dai Yan, Li Jie, Yu Xiaoliang, Wang Chengyong, Wang Xinyu, Zhang Zhichao, 2023. Metallogenic Characteristics of Langmuri Copper Polymetallic Deposit in East Kunlun and Its Ore Prospecting Enlightenment. Earth Science, 48(12): 4349-4369. doi: 10.3799/dqkx.2023.028

Citation:

Tong Haikui, Long Lingli, Wang Yuwang, Zhu Xinyou, Li Shunting, Gu Zicheng, Ma Cai, Dai Yan, Li Jie, Yu Xiaoliang, Wang Chengyong, Wang Xinyu, Zhang Zhichao, 2023. Metallogenic Characteristics of Langmuri Copper Polymetallic Deposit in East Kunlun and Its Ore Prospecting Enlightenment. Earth Science, 48(12): 4349-4369. doi: 10.3799/dqkx.2023.028

Citation:

Tong Haikui, Long Lingli, Wang Yuwang, Zhu Xinyou, Li Shunting, Gu Zicheng, Ma Cai, Dai Yan, Li Jie, Yu Xiaoliang, Wang Chengyong, Wang Xinyu, Zhang Zhichao, 2023. Metallogenic Characteristics of Langmuri Copper Polymetallic Deposit in East Kunlun and Its Ore Prospecting Enlightenment. Earth Science, 48(12): 4349-4369. doi: 10.3799/dqkx.2023.028

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Metallogenic Characteristics of Langmuri Copper Polymetallic Deposit in East Kunlun and Its Ore Prospecting Enlightenment

doi: 10.3799/dqkx.2023.028

Tong Haikui^{1, 2
,
,},
Long Lingli^{3, 4
,
,},
Wang Yuwang^{3, 4},
Zhu Xinyou^{3, 4},
Li Shunting^{3, 4},
Gu Zicheng^{3, 4},
Ma Cai^{1, 2},
Dai Yan^{1, 2},
Li Jie^{1, 2},
Yu Xiaoliang^{1, 2},
Wang Chengyong^{1, 2},
Wang Xinyu^{3, 4},
Zhang Zhichao^{3, 4}

1.
Geological Survey Bureau of Qinghai Province, Xining, 810001, China
2.
Technology Innovation Center for Exploration and Exploitation of Strategic Mineral Resources in Plateau Desert Region, Ministry of Natural Resources, Xining, 810001, China
3.
Beijing Institute of Geology for Mineral Resources, Beijing 100012, China
4.
Technic Research Center for Deep Resources Exploration in Non-Ferrous Metal Mines, Beijing 100012, China

Received Date: 2022-12-13
Publish Date: 2023-12-25

Abstract

Abstract

The Langmuri Cu-Ni-Co polymetallic deposit, located in the eastern segment of the eastern Kunlun orogenic belt, has recently delineated an independent platinum group element orebody. Further study on the metallogenic characteristics of the deposit is helpful to guide the further exploration work. Based on the analysis of the geological characteristics of the deposit, combined the analysis of the major and trace elements, Sr-Nd isotopes of the ore-bearing olivine pyroxenolite and the electron-probe microanalysis of major elements in olivine and mica from the ore-bearing olivine pyroxenolite, as well as the zircon U-Pb chronology and geochemistry of the biotite granite, In this paper it discusses the metallogenic characteristics, metallogenic age and genesis of the Langmuri deposit. Olivine in ore-bearing olivine pyroxenolite belongs to chrysolite series (Fo value is 86.72-88.39), and mica is phlogopite, which are all products of mantle-derived magmatism. The geochemical characters of the ore-bearing olivine pyroxene show a right-dipping REE distribution patterns, enriched with LILE elements such as Cs, Rb, U, etc., and with positive ε_Nd(t) values of 0.66-2.66, suggest that the parent magma of olivine pyroxene experienced crustal contamination during its formation. The age of biotite granite is 414.5 ± 8.8 Ma, which shows the geochemical characteristics of arc magma.(⁸⁷Sr/⁸⁶Sr)_i(0.718 609-0.719 177) and ε_Nd(t) values (1.28-5.36) show that the biotite granite is the product of crust- mantle magma mixing. In this paper it proposes that Langmuri copper-polymetallic deposit underwent multi-period of superimposed mineralization. The Cu-Ni-Co-Pt-Pd sulfide orebodies hosted in olivine pyroxenolite were formed at 450-439 Ma, and the hydrothermal vein-type copper mineralization related to biotite granite with 415 Ma was superimposed upon it. The deposit is dominated by early sulfide mineralization related to olivine pyroxene. Crustal contamination in the process of magmatic evolution and post-magmatic hydrothermal activities have important contributions to mineralization.The bottom and top of the basic-ultrabasic complex in Langmuri mining area and the contact zone between biotite granite and it are all favorable prospecting areas.
- East Kunlun,
- Langmuri,
- magmatic sulfide deposit,
- superimposed mineralization,
- copper-polymetallic deposit,
- metallogenic characteristics

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References(115)

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Metallogenic Characteristics of Langmuri Copper Polymetallic Deposit in East Kunlun and Its Ore Prospecting Enlightenment

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