粤西晚侏罗世花岗质岩体及其暗色微粒包体的成因及意义：年代学、矿物学和地球化学约束

刘梓; 张玉芝; 崔翔; 甘成势; 王岳军

doi:10.3799/dqkx.2019.113

Volume 45 Issue 4

Apr. 2020

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Article Navigation > Earth Science > 2020 > 45(4): 1243-1265

Liu Zi, Zhang Yuzhi, Cui Xiang, Gan Chengshi, Wang Yuejun, 2020. Petrogenesis and Implications of the Late Jurassic Granitoid and Its Mafic Microgranular Enclaves in West Guangdong Province: Constraints from Geochronological, Mineralogical and Geochemical Evidence. Earth Science, 45(4): 1243-1265. doi: 10.3799/dqkx.2019.113

Citation:

Liu Zi, Zhang Yuzhi, Cui Xiang, Gan Chengshi, Wang Yuejun, 2020. Petrogenesis and Implications of the Late Jurassic Granitoid and Its Mafic Microgranular Enclaves in West Guangdong Province: Constraints from Geochronological, Mineralogical and Geochemical Evidence. Earth Science, 45(4): 1243-1265. doi: 10.3799/dqkx.2019.113

Citation:

Liu Zi, Zhang Yuzhi, Cui Xiang, Gan Chengshi, Wang Yuejun, 2020. Petrogenesis and Implications of the Late Jurassic Granitoid and Its Mafic Microgranular Enclaves in West Guangdong Province: Constraints from Geochronological, Mineralogical and Geochemical Evidence. Earth Science, 45(4): 1243-1265. doi: 10.3799/dqkx.2019.113

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Petrogenesis and Implications of the Late Jurassic Granitoid and Its Mafic Microgranular Enclaves in West Guangdong Province: Constraints from Geochronological, Mineralogical and Geochemical Evidence

doi: 10.3799/dqkx.2019.113

Liu Zi^{1
,
,},
Zhang Yuzhi^{1, 2, 3
,
,},
Cui Xiang^{1, 2, 3},
Gan Chengshi^{1, 2, 3},
Wang Yuejun^{1, 2, 3}

1.
School of Earth Sciences and Engineering, Sun Yat-sen University, Guangzhou 510275, China
2.
Guangdong Provincial Key Laboratory of Geodynamics and Geohazards, Guangzhou 510275, China
3.
Southern Laboratory of Ocean Science and Engineering, Zhuhai 519082, China

Received Date: 2019-05-19
Publish Date: 2020-04-15

Abstract

Abstract

Mafic microgranular enclaves (MMEs) are widespread in the host granitoid from the Ba'er pluton in the west of the Guangdong Province. The MMEs have variable shapes and share similar mineral compositions with their host rocks, but are not fully understood. Petrographic study, zircon U-Pb dating and geochemical data are reported for the host granitoid and its MMEs, to constrain their petrogenesis and tectonic setting. LA-ICP-MS zircon U-Pb dating results yield weighted mean ²³⁸U/²⁰⁶Pb ages of 160.0±1.0 Ma and 159.3±1.1 Ma for the host rocks and the MMEs, respectively. The host granitoid is characterized by high SiO₂(61.04%-65.84%), K₂O(1.60%-4.97%), low A/CNK(1.59-1.99), belonging to metaluminous, K-enriched I-type granitoid. Both host rocks and MMEs are enriched in LREE and LILE, and are depleted in HREE and HFSE (e.g., Nb, Ta and Ti). In addition, they also have indistinguishable Sr-Nd isotopic compositions. The granitoid has ε_Nd(t) values of -5.73 to -5.67 and (⁸⁷Sr/⁸⁶Sr)_i values of 0.707 63-0.707 67. The MMEs have ε_Nd(t) values of -5.81 to -4.35 and (⁸⁷Sr/⁸⁶Sr)_i values of 0.707 04-0.707 74. The calculated crystallization temperatures and depths of the Ba'er pluton are 730-754℃ and 16.8-20.6 km, respectively. According to comprehensive analysis of their tectonic settings as well as petrographic characteristics and geochemical data, the magma produced by partial melting of predominantly mafic middle-lower crust, with the input of minor mantle-derived materials, experienced different degrees of fractional crystallization in an intraplate extensional setting of Late Jurassic, Southeast China, which was accompanied by local magma mixing. The MMEs are generated by the mixing of the mafic magma with felsic magma.
- South China,
- Late Jurassic,
- mafic microgranular enclave,
- U-Pb ages,
- geochemistry

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References(155)

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Petrogenesis and Implications of the Late Jurassic Granitoid and Its Mafic Microgranular Enclaves in West Guangdong Province: Constraints from Geochronological, Mineralogical and Geochemical Evidence

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