阿尔泰造山带南缘岩浆混合作用：阿克布拉克岩体岩石学、地球化学和年代学证据

蔺新望; 张亚峰; 陈国超; 郭岐明; 王星; 赵端昌

doi:10.3799/dqkx.2021.215

Volume 48 Issue 10

Oct. 2023

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Lin Xinwang, Zhang Yafeng, Chen Guochao, Guo Qiming, Wang Xing, Zhao Duanchang, 2023. LA-ICP-MS U-Pb Geochronology, Geochemistry and Petrography of Akebulake Pluton in Southern Altay Orogenic Belt: An Example for Magma Mixing. Earth Science, 48(10): 3597-3612. doi: 10.3799/dqkx.2021.215

Citation:

Lin Xinwang, Zhang Yafeng, Chen Guochao, Guo Qiming, Wang Xing, Zhao Duanchang, 2023. LA-ICP-MS U-Pb Geochronology, Geochemistry and Petrography of Akebulake Pluton in Southern Altay Orogenic Belt: An Example for Magma Mixing. Earth Science, 48(10): 3597-3612. doi: 10.3799/dqkx.2021.215

Citation:

Lin Xinwang, Zhang Yafeng, Chen Guochao, Guo Qiming, Wang Xing, Zhao Duanchang, 2023. LA-ICP-MS U-Pb Geochronology, Geochemistry and Petrography of Akebulake Pluton in Southern Altay Orogenic Belt: An Example for Magma Mixing. Earth Science, 48(10): 3597-3612. doi: 10.3799/dqkx.2021.215

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LA-ICP-MS U-Pb Geochronology, Geochemistry and Petrography of Akebulake Pluton in Southern Altay Orogenic Belt: An Example for Magma Mixing

doi: 10.3799/dqkx.2021.215

1.
Shaanxi Mineral Resources and Geological Survey, Xi'an 710068, China
2.
School of Civil Engineering, Nanyang Institute of Technology, Nanyang 473000, China
3.
Key Laboratory of Western China's Mineral Resources and Geological Engineering, Ministry of Education, Chang'an University, Xi'an 710054, China

Received Date: 2021-09-17
Available Online: 2023-10-31
Publish Date: 2023-10-25

Abstract

Abstract

The Akebulake pluton in the southern margin of the Altay orogenic belt is composed of tonalite, dioritic microgranular enclaves and mafic dikes. The pluton exhibits excellent evidence for magma mixing and mingling, such as the feldspathic phenocryst, long prisms of apatite in enclaves and quartz, plagioclase wrapped in biotite in the host rock. Host rocks, dioritic microgranular enclaves and mafic dikes of the Akebulake pluton are products of mixing with different end element ratios in the process of magma mixing evolution. LA-ICP-MS zircon U-Pb dating from three samples yielded weighted mean ²⁰⁶Pb/²³⁸U ages of 396.3±3.3 Ma, 392.2±3.7 Ma and 402.3±3.3 Ma, respectively. It indicates that they were formed in the same magmatic event, which provides important chronological evidence for the genesis of magma mixing of Akebulake pluton. Geochemically, the major oxide content of the mafic dikes, dioritic enclaves and their host rocks all have a good linear relationship in the plot, and the patterns of REE, spidergrams of trace elements of the dioritic enclaves and mafic dikes are similar to those of the host granites, suggesting that component exchange and homogenization occurred between the enclaves and the host rocks in the process of rock formation. Hf isotopic composition of zircon is not uniform. The host rocks, enclaves and mafic dikes ε_Hf(t) vary from 1.22 to 4.70, -3.49 to 7.41 and 3.65 to 9.02, respectively. The Hf isotopic model ages (t_DM2) range from 962 to 1 131 Ma, 816 to 1 375 Ma and 740 to 1 015 Ma, respectively. Based on a comprehensive analysis with the data of southern margin of Altay, the authors hold that the dioritic enclaves in the Akebulake pluton were generated by mixing of mantle-derived mafic magma and its induced crustal felsic magma in an island-arc setting of active continental margin. The formation of magma mixing of the Akebulake pluton further confirms that strong crust-mantle magmatic mixing occurred in the deep crust of the southern margin of the Altay orogenic belt during the Early Devonian, which resulted in an important event of lateral continental crust growth at the syn-accretionary stage in Altay.
- LA-ICP-MS zircon U-Pb age,
- magma mixing,
- mafic microgranular enclave,
- Akebulake pluton,
- altay,
- geochemistry,
- petrology

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References(91)

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LA-ICP-MS U-Pb Geochronology, Geochemistry and Petrography of Akebulake Pluton in Southern Altay Orogenic Belt: An Example for Magma Mixing

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