豫西火神庙岩体锆石U-Pb年代学、地球化学及Hf同位素组成

王赛; 叶会寿; 杨永强; 张兴康; 苏慧敏; 杨晨英

doi:10.3799/dqkx.2016.022

Volume 41 Issue 2

Feb. 2016

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Article Navigation > Earth Science > 2016 > 41(2): 293-316

Wang Sai, Ye Huishou, Yang Yongqiang, Zhang Xingkang, Su Huimin, Yang Chenying, 2016. Zircon U-Pb Chronology, Geochemistry and Hf Isotopic Compositions of the Huoshenmiao Pluton, Western Henan. Earth Science, 41(2): 293-316. doi: 10.3799/dqkx.2016.022

Citation:

Wang Sai, Ye Huishou, Yang Yongqiang, Zhang Xingkang, Su Huimin, Yang Chenying, 2016. Zircon U-Pb Chronology, Geochemistry and Hf Isotopic Compositions of the Huoshenmiao Pluton, Western Henan. Earth Science, 41(2): 293-316. doi: 10.3799/dqkx.2016.022

Citation:

Wang Sai, Ye Huishou, Yang Yongqiang, Zhang Xingkang, Su Huimin, Yang Chenying, 2016. Zircon U-Pb Chronology, Geochemistry and Hf Isotopic Compositions of the Huoshenmiao Pluton, Western Henan. Earth Science, 41(2): 293-316. doi: 10.3799/dqkx.2016.022

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Zircon U-Pb Chronology, Geochemistry and Hf Isotopic Compositions of the Huoshenmiao Pluton, Western Henan

doi: 10.3799/dqkx.2016.022

1.
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China
2.
MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, China Academy of Geological Sciences, Beijing 100037, China
3.
Hebei Institute of Geological Survey, Shijiazhuang 050081, China
4.
School of Earth Sciences, China University of Geosciences, Wuhan 430074, China

Received Date: 2015-07-21
Publish Date: 2016-02-15

Abstract

Abstract

The Huoshenmiao pluton located in the west of the Luanchuan ore district, southern margin of the North China Craton (NCC) is mainly composed of quartz diorite, monzo-granite and granite porphyry. The Huoshenmiao pluton is closely related to the Huoshenmiao Mo deposit. While the degree of research on the Huoshenmiao pluton is very low, which seriously restrict the understanding of the genesis of the Huoshenmiao Mo deposit. Three types of rock including quartz diorite, monzo-granite and granite porphyry has been researched by zircon U-Pb chronology, geochemistry and Hf isotope. The forming ages of quartz diorite, monzo-granite and granite porphyry are 150.3±0.6Ma, 146.0±0.6Ma and 145.1±0.5Ma respectively, and are products of the second magmatism of the Luanchuan ore district, Late Jurassic. Geochemistry and zircon Hf isotope show that the Huoshenmiao pluton belongs to I-type granite, and it results from ascending magma formed by partial melting of different source regions. The quartz diorite stems from remelting of the enriched mantle, while the monzo-granite and granite porphyry are the products of mafic magma derived from remelting of the enriched mantle mixed with felsic magma derived from remelting of the Taihua TTG.
- zircon U-Pb chronology,
- geochemistry,
- Hf isotope,
- Huoshenmiao pluton,
- West Henan

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References(137)

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