集宁地区两类古元古代重熔花岗岩的锆石U-Pb年代学及岩石成因

常青松; 王惠初; 施建荣; 任云伟

doi:10.3799/dqkx.2020.135

Volume 45 Issue 9

Sep. 2020

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Article Navigation > Earth Science > 2020 > 45(9): 3258-3267

Chang Qingsong, Wang Huichu, Shi Jianrong, Ren Yunwei, 2020. Zircon U-Pb Chronology and Petrogenesis of Two Types of Remelting Granite in Jining Area. Earth Science, 45(9): 3258-3267. doi: 10.3799/dqkx.2020.135

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Chang Qingsong, Wang Huichu, Shi Jianrong, Ren Yunwei, 2020. Zircon U-Pb Chronology and Petrogenesis of Two Types of Remelting Granite in Jining Area. Earth Science, 45(9): 3258-3267. doi: 10.3799/dqkx.2020.135

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Zircon U-Pb Chronology and Petrogenesis of Two Types of Remelting Granite in Jining Area

doi: 10.3799/dqkx.2020.135

Chang Qingsong^{1, 2
,
,},
Wang Huichu^{1, 2},
Shi Jianrong^{1, 2},
Ren Yunwei^{1, 2}

1.
Tianjin Center, China Geological Survey, Tianjin 300170, China
2.
Pre-Cambrian Geological Research Center, China Geological Survey, Tianjin 300170, China

Received Date: 2020-04-02
Publish Date: 2020-09-15

Abstract

Abstract

The petrogenesis of Paleoproterozoic remelting granite in Jining-Liangcheng area has been interpreted differently in academia. Geochronologic and geochemical studies of two types of remelting granite are presented in this paper. Zircon LA-MC-ICP-MS U-Pb isotopic dating reveals that the porphyritic charnockites emplaced at 1 954 Ma and were metamorphosed at 1 827 Ma, and the meta-leucogranites emplaced at 1 956 Ma. The porphyritic charnockites are characterized by low Si contents, high Fe and Mg contents, with negative Eu anomalies and relative depletion of Sr. The meta-leucogranites have high content of Si and low contents of Fe and Mg, strong depletion in high filed-strength elements (HFSE, such as Nb, Ta and Ti) and enrichment in large iron lithophile elements (LILE, such as K, Rb and Ba). Both two types of granite were generated in the same period, from the remelting associated with mantle-source magma underplating. The source magma of the porphyritic charnockites was mixed with certain amount of mantle contribution during remelting of meta-sediments of khondalite series, before fractional crystallization. And the source magma of the meta-leucogranites was generated mainly from remelting of meta-sediments of khondalite series, with limited influence of mantle contribution.
- remelting granite,
- Paleoproterozoic,
- zircon U-Pb chronology,
- geochemistry

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References(48)

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