黑龙江省翠中铁钨多金属矿床成岩成矿年代学、地球化学特征及地质意义

杨健; 胡新露; 李春芳; 董子良; 曾国平; 姚书振

doi:10.3799/dqkx.2019.190

Volume 45 Issue 5

May 2020

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Yang Jian, Hu Xinlu, Li Chunfang, Dong Ziliang, Zeng Guoping, Yao Shuzhen, 2020. Petrogenic and Metallogenic Geochronology, Geochemical Characteristics and Its Geological Implications of Cuizhong Fe Polymetallic Deposit, Heilongjiang Province. Earth Science, 45(5): 1593-1608. doi: 10.3799/dqkx.2019.190

Citation:

Yang Jian, Hu Xinlu, Li Chunfang, Dong Ziliang, Zeng Guoping, Yao Shuzhen, 2020. Petrogenic and Metallogenic Geochronology, Geochemical Characteristics and Its Geological Implications of Cuizhong Fe Polymetallic Deposit, Heilongjiang Province. Earth Science, 45(5): 1593-1608. doi: 10.3799/dqkx.2019.190

Citation:

Yang Jian, Hu Xinlu, Li Chunfang, Dong Ziliang, Zeng Guoping, Yao Shuzhen, 2020. Petrogenic and Metallogenic Geochronology, Geochemical Characteristics and Its Geological Implications of Cuizhong Fe Polymetallic Deposit, Heilongjiang Province. Earth Science, 45(5): 1593-1608. doi: 10.3799/dqkx.2019.190

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Petrogenic and Metallogenic Geochronology, Geochemical Characteristics and Its Geological Implications of Cuizhong Fe Polymetallic Deposit, Heilongjiang Province

doi: 10.3799/dqkx.2019.190

1.
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
2.
Heilongjiang Mining Group Co., Ltd., Harbin 150036, China
3.
Wuhan Center, China Geological Survey, Wuhan 430205, China

Received Date: 2019-08-02
Publish Date: 2020-05-15

Abstract

Abstract

Two main types of igneous rocks are distributed in the Cuizhong Fe polymetallic deposit, including the coarse-grained alkali-feldspar granite in the shallow part and the fine-grained alkali-feldspar granite at depth, whose relationships with ore mineralization have long been debated. Whole rock geochemistry, zircon U-Pb geochronology and Hf isotopic analyses are carried out for these two types of granitoids. Pb isotopic analyses are performed on both the granitoids and the sulfides. The coarse-grained alkali-feldspar granite and fine-grained alkali-feldspar granite yield weighted mean ²⁰⁶Pb/²³⁸U age of 503±2.9 Ma and 201±6.4 Ma respectively, indicating that they were formed during middle Caledonian and late Indosinian-early Yanshanian respectively.The Re-Os model age of molybdenite is 202±2.9 Ma, which is consistent with the crystallization age of the fine-grained alkali-feldspar granite.Zircons in the coarse-grained alkali-feldspar granite display ε_Hf(t) values of -8.31 to 0.57, indicating that it was derived from partial melting of Mesoproterozoic crustal rocks. Zircon crystals in the fine-grained alkali-feldspar granite have ε_Hf(t) values of 2.84 to 4.78, indicating that it was generated by reworking of newly-growing juvenile crustal material which was originated from depleted mantle. In combination with the metallogenic and petrologic ages, trend surface analysis of ore-forming elements, and the comparison of Pb isotopes, we suggest that the mineralization in the Cuizhong Fe polymetallic deposit is genetically associated with the fine-grained alkali-feldspar granite. The polymetallic mineralization was generated in a compressional tectonic setting in response to the subduction of the Jiamusi Block towards the Songnen Block.
- skarn-type deposit,
- zircon U-Pb geochronology,
- zircon Hf isotope,
- Cuizhong Fe polymetallic deposit,
- lesser Xing'an-Zhangguangcai metallogenic belt,
- geochemistry

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References(56)

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