湘中紫云山岩体暗色微粒包体的成因：岩相学、全岩及矿物地球化学证据

曾认宇; 赖健清; 张利军; 鞠培姣

doi:10.3799/dqkx.2016.512

Volume 41 Issue 9

Sep. 2016

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Article Navigation > Earth Science > 2016 > 41(9): 1461-1478

Zeng Renyu, Lai Jianqing, Zhang Lijun, Ju Peijiao, 2016. Petrogenesis of Mafic Microgranular Enclaves: Evidence from Petrography, Whole-Rock and Mineral Chemistry of Ziyunshan Pluton, Central Hunan. Earth Science, 41(9): 1461-1478. doi: 10.3799/dqkx.2016.512

Citation:

Zeng Renyu, Lai Jianqing, Zhang Lijun, Ju Peijiao, 2016. Petrogenesis of Mafic Microgranular Enclaves: Evidence from Petrography, Whole-Rock and Mineral Chemistry of Ziyunshan Pluton, Central Hunan. Earth Science, 41(9): 1461-1478. doi: 10.3799/dqkx.2016.512

Citation:

Zeng Renyu, Lai Jianqing, Zhang Lijun, Ju Peijiao, 2016. Petrogenesis of Mafic Microgranular Enclaves: Evidence from Petrography, Whole-Rock and Mineral Chemistry of Ziyunshan Pluton, Central Hunan. Earth Science, 41(9): 1461-1478. doi: 10.3799/dqkx.2016.512

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Petrogenesis of Mafic Microgranular Enclaves: Evidence from Petrography, Whole-Rock and Mineral Chemistry of Ziyunshan Pluton, Central Hunan

doi: 10.3799/dqkx.2016.512

Zeng Renyu^{1,2
,},
Lai Jianqing^{1,2
,
,},
Zhang Lijun^1,2,3,
Ju Peijiao^1,2

1.
Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring, Ministry of Education, Central South University, Changsha 410083, China
2.
School of Geosciences and Info-Physics, Central South University, Changsha 410083, China
3.
Institute of Hunan Nonferrous Geological Exploration, Changsha 410015, China

Received Date: 2016-01-22
Publish Date: 2016-09-15

Abstract

Abstract

The porphyraceous hornblende biotite granodiorite is generated in the Ziyunshan pluton, Central Hunan Province, which hosts many mafic microgranular enclaves (MMEs). This paper presents petrography, major and trace elements of whole-rock, and mineral chemistry of feldspar, pyroxene, as well as biotite of the igneous-texture mafic microgranular enclaves and host rocks, their genetic mechanism and geotectonic significance were investigated. The whole-rock geochemistry of host rocks is more stable than those of mafic microgranular enclaves, and the latter were characterized by relatively depleted SiO₂ and enriched Na₂O. Both of them are represented by metaluminous, calc-alkaline and magnesian, and enrichment of LREE and LILE and depletion of HREE and HFSE. The plagioclase, pyroxene and biotite of host rocks and mafic microgranular enclaves belong to andesine, ferrosalite-salite and ferribiotite, respectively, showing similar characteristics of mineral chemistry. According to a comprehensive analysis of petrographical characteristics and geochemical data, it is suggested that (1) the host rock belongs to I-type and ACG-type granite, showing the characteristics of crust-mantle mixing; (2) the mafic microgranular enclaves were formed in liquid state, having liquidity and featuring both mechanical and chemical interactions with host rocks; (3) the crystallization of the mafic microgranular enclaves can be classified into two stages: the initial one is undercooling and rapid crystallization stage, and the latter is slow crystallization stage. To sum up, the mafic microgranular enclaves in the Ziyunshan pluton were generated by mixing of mafic magmas (sub-alkaline tholeiite which formed from mantle) and its induced crustal felsic magma (products of partial melting of arenaceous rock in crust) in the relaxation period after the compressive stress period in the late Indo-Chinese epoch.
- Ziyunshan pluton,
- mafic microgranular enclave,
- mineral,
- geochemistry,
- magma mixing,
- pyroxene,
- igneous rock

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References(79)

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Petrogenesis of Mafic Microgranular Enclaves: Evidence from Petrography, Whole-Rock and Mineral Chemistry of Ziyunshan Pluton, Central Hunan

doi: 10.3799/dqkx.2016.512

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