造山带铜镍硫化物矿床的岩浆起源：以东天山黄山南铜镍矿床为例

王旋; 曹俊; 张盖之

doi:10.3799/dqkx.2021.015

Volume 46 Issue 11

Nov. 2021

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Article Navigation > Earth Science > 2021 > 46(11): 3829-3849

Wang Xuan, Cao Jun, Zhang Gaizhi, 2021. Origin of Ore-Forming Magmas Associated with Ni-Cu Sulfide Deposits in Orogenic Belts: Case Study of Permian Huangshannan Magmatic Ni-Cu Sulfide Deposit, East Tianshan, NW China. Earth Science, 46(11): 3829-3849. doi: 10.3799/dqkx.2021.015

Citation:

Wang Xuan, Cao Jun, Zhang Gaizhi, 2021. Origin of Ore-Forming Magmas Associated with Ni-Cu Sulfide Deposits in Orogenic Belts: Case Study of Permian Huangshannan Magmatic Ni-Cu Sulfide Deposit, East Tianshan, NW China. Earth Science, 46(11): 3829-3849. doi: 10.3799/dqkx.2021.015

Citation:

Wang Xuan, Cao Jun, Zhang Gaizhi, 2021. Origin of Ore-Forming Magmas Associated with Ni-Cu Sulfide Deposits in Orogenic Belts: Case Study of Permian Huangshannan Magmatic Ni-Cu Sulfide Deposit, East Tianshan, NW China. Earth Science, 46(11): 3829-3849. doi: 10.3799/dqkx.2021.015

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Origin of Ore-Forming Magmas Associated with Ni-Cu Sulfide Deposits in Orogenic Belts: Case Study of Permian Huangshannan Magmatic Ni-Cu Sulfide Deposit, East Tianshan, NW China

doi: 10.3799/dqkx.2021.015

Wang Xuan^{1, 3
,
,},
Cao Jun^{1, 2, 3
,
,
,},
Zhang Gaizhi^{1, 3}

1.
State Key Laboratory of Nuclear Resources and Environment, East China University of Technology, Nanchang 330013, China
2.
Key Laboratory of Tectonic Controlled Mineralization and Oil Reservoir of Ministry of Natural Resources, Chengdu University of Technology, Chengdu 610059, China
3.
School of Earth Sciences, East China University of Technology, Nanchang 330013, China

Received Date: 2021-02-03
Available Online: 2021-12-04
Publish Date: 2021-11-30

Abstract

Abstract

The East Tianshan is situated along the southern margin of the Central Asian Orogenic Belt, and its outcrops of a series of important magmatic Ni-Cu sulfide deposits hosted by mafic-ultramafic intrusions are the focus of recent studies. In this study, it presents a systematic study of petrology, mineralogy and geochemistry of the Huangshannan sulfide ore-bearing mafic-ultramafic intrusion of the East Tianshan region, in order to further discuss the origin and nature of its parental magma. The Huangshannan intrusion consists of an ultramafic unit, which is composed of harzburgite, lherzolite and olivine websterite, and a mafic unit, which is composed of (olivine) gabbronorite and diorite. The rocks of the intrusion are characterized by enrichments of large ion lithophile elements, light rare earth elements and strong negative Nb-Ta, Ti anomalies, similar to that of typical arc volcanics. These rocks also have variable isotope compositions[ε_Nd(t=282.5 Ma)=(-1.31)-4.22;(⁸⁷Sr/⁸⁶Sr)_i=0.703 2-0.706 9;(²⁰⁶Pb/²⁰⁴Pb)_i=17.67-18.90], indicating the parental magma was derived from a moderately enriched depleted mantle source and contaminated by 5%-20% juvenile arc crust and then by ~5% upper crustal materials. According to its highest Fo olivine, the estimated parental magma of the Huangshannan intrusion has 12.11% MgO, 11.14% FeO_Total and 306×10^-6 Ni, indicating the picritic magma was generated from partial melting of both the asthenosphere and mantle wedge. The low Ca (< 725×10^-6), 100×Mn/Fe (1.18-1.38) and high Ni (1 451×10^-6-2 813×10^-6), Mn/Zn (11.09-23.53) ratios of the Huangshannan olivines indicate the Huangshannan parental magma may be derived from pyroxenite in a modally enriched peridotite mantle source. Therefore, it speculates that the Huangshannan primary magmas were likely derived from a lithospheric pyroxenite mantle source as the result of slab-derived fluid modification during previous subduction.
- Central Asian Orogenic Belt,
- East Tianshan,
- mafic-ultramafic intrusion,
- Ni-Cu sulfide deposit,
- pyroxenite,
- ore deposit

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References(96)

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