华南桂东南地区加里东期Ⅰ型花岗岩类的岩石成因及构造意义

刘明辉; 时毓; 唐远兰; 赵增霞; 刘希军; 高爱洋; 黄椿文

doi:10.3799/dqkx.2021.035

Volume 46 Issue 11

Nov. 2021

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Article Navigation > Earth Science > 2021 > 46(11): 3965-3992

Liu Minghui, Shi Yu, Tang Yuanlan, Zhao Zengxia, Liu Xijun, Gao Aiyang, Huang Chunwen, 2021. Petrogenesis and Tectonic Significance of Caledonian Ⅰ-Type Granitoids in Southeast Guangxi, South China. Earth Science, 46(11): 3965-3992. doi: 10.3799/dqkx.2021.035

Citation:

Liu Minghui, Shi Yu, Tang Yuanlan, Zhao Zengxia, Liu Xijun, Gao Aiyang, Huang Chunwen, 2021. Petrogenesis and Tectonic Significance of Caledonian Ⅰ-Type Granitoids in Southeast Guangxi, South China. Earth Science, 46(11): 3965-3992. doi: 10.3799/dqkx.2021.035

Citation:

Liu Minghui, Shi Yu, Tang Yuanlan, Zhao Zengxia, Liu Xijun, Gao Aiyang, Huang Chunwen, 2021. Petrogenesis and Tectonic Significance of Caledonian Ⅰ-Type Granitoids in Southeast Guangxi, South China. Earth Science, 46(11): 3965-3992. doi: 10.3799/dqkx.2021.035

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Petrogenesis and Tectonic Significance of Caledonian Ⅰ-Type Granitoids in Southeast Guangxi, South China

doi: 10.3799/dqkx.2021.035

Liu Minghui^{1, 2
,
,},
Shi Yu^{1, 2, 3
,
,},
Tang Yuanlan^{1, 2},
Zhao Zengxia^{1, 2},
Liu Xijun^{1, 2},
Gao Aiyang^{1, 2},
Huang Chunwen^{1, 2}

1.
Guangxi Key Laboratory of Hidden Metallic Ore Deposits Exploration, Guilin University of Technology, Guilin 541004, China
2.
Collaborative Innovation Center for Exploration of Nonferrous Metal Deposits and Efficient Utilization of Resources, Guilin University of Technology, Guilin 541004, China
3.
State Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing 210093, China

Received Date: 2021-02-09
Available Online: 2021-12-04
Publish Date: 2021-11-30

Abstract

Abstract

The Longxin and Xiaying plutons are located in the southwest of the Yangtze and Cathaysia blocks collision belt, studying the petrogenesis of the Ⅰ-type granitoids is of great geological significance to reveal the geodynamic background and tectonic evolution of the Early Paleozoic in Southeast Guangxi. LA-ICP-MS zircon U-Pb dating, geochemical and Lu-Hf isotopic data are reported for the host rock and its mafic microgranular enclave (MME) of Longxin and Xiaying plutons. Zircon U-Pb dating results of samples from the Longxin and Xiaying plutons show that the age of the host rock (granodiorite) of the Longxin pluton is 440±2 Ma, and that of the MME (diorite) of the Longxin pluton is 441±1 Ma, showing that the host rock and the MMEs are the products of the simultaneous magmatism. The age of the granodiorite and monzogranite of Xiaying pluton are 447±3 Ma and 436±3 Ma, indicating that there were at least two stages of intrusion in the Xiaying pluton. Both the host rocks (granodiorite) and MME (diorite) of the Longxin pluton have negative ε_Hf(t) values (-3.32 to -5.83 and -17.89 to -1.82), and the corresponding two-stage model ages (T_DM2) are 1.62-1.76 Ga and 1.57-2.54 Ga, respectively. The zircon ε_Hf(t) values of the granodiorite (early stage) and monzogranite (late stage) of the Xiaying pluton are -15.43 to 3.03 and -4.79 to 6.82, respectively, with the T_DM2 model ages of 1.59-1.99 Ga and 0.97-1.70 Ga, respectively, indicating that the parental magma of the granitic rocks might have originated mainly from crustal materials of the Paleoproterozoic-Mesoproterozoic. Geochemical data exhibit that the host rocks of the Longxin pluton are peraluminous high-K calc-alkaline Ⅰ-type granite, with relatively high light rare earth elements (LREE) and large ion lithophile elements (LILE), with low high field strength elements (HFSE) and heavy rare earth elements (HREE). For the Xiaying pluton, the granodiorite (early stage) is weakly peraluminous high-K calc-alkaline Ⅰ-type granite, while the monzogranite (late stage) is peraluminous high-K calc-alkaline Ⅰ-type granite, which is similar to the host rocks of the Longxin pluton. According to the petrography, geochronology, geochemistry and Hf isotopic composition characteristics of granites and mafic inclusions in the study area, indicating the MME (diorite) of Longxin formed by the magma mingling and mixing, although the host rock (granodiorite) of the Longxin and Xiaying plutons (granodiorite and monzogranite) have similar sources and petrogenesis, which have differences in magma mixing and fractional crystallization in the formation of granites. Based on previous studies on the tectonic setting in South China, it is suggested that the Longxin and Xiaying plutons were formed by the extension and thinning of the lithosphere, upwelling and underplating of the hot mantle-derived magma after the intra-continental orogeny of the Yangtze and Cathaysia blocks. The lower crust was partially melted under the influence of mantle heat and formed the acid magma, and then mixed with the mafic magma for limited and uneven degrees of crust-mantle mixing in the source region.
- Caledonian,
- Ⅰ-type granitoid,
- zircon geochronology,
- Longxin and Xiaying plutons,
- Southeast Guangxi,
- geochemistry,
- petrology

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References(137)

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Petrogenesis and Tectonic Significance of Caledonian Ⅰ-Type Granitoids in Southeast Guangxi, South China

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