东昆仑东段哈拉尕吐花岗岩基岩浆混合作用:来自岩石学和矿物学约束

陈国超; 裴先治; 李瑞保; 李佐臣; 裴磊; 刘成军; 陈有炘; 王盟; 张玉; 李小兵

doi:10.3799/dqkx.2018.559

Volume 43 Issue 9

Sep. 2018

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Article Navigation > Earth Science > 2018 > 43(9): 3200-3217

Chen Guochao, Pei Xianzhi, Li Ruibao, Li Zuochen, Pei Lei, Liu Chengjun, Chen Youxin, Wang Meng, Zhang Yu, Li Xiaobing, 2018. Magma Mixing in Halagatu Granitic Batholith from Eastern Part of the East Kunlun Orogenic Belt: Constraints from Lithology and Mineralogy. Earth Science, 43(9): 3200-3217. doi: 10.3799/dqkx.2018.559

Citation:

Chen Guochao, Pei Xianzhi, Li Ruibao, Li Zuochen, Pei Lei, Liu Chengjun, Chen Youxin, Wang Meng, Zhang Yu, Li Xiaobing, 2018. Magma Mixing in Halagatu Granitic Batholith from Eastern Part of the East Kunlun Orogenic Belt: Constraints from Lithology and Mineralogy. Earth Science, 43(9): 3200-3217. doi: 10.3799/dqkx.2018.559

Citation:

Chen Guochao, Pei Xianzhi, Li Ruibao, Li Zuochen, Pei Lei, Liu Chengjun, Chen Youxin, Wang Meng, Zhang Yu, Li Xiaobing, 2018. Magma Mixing in Halagatu Granitic Batholith from Eastern Part of the East Kunlun Orogenic Belt: Constraints from Lithology and Mineralogy. Earth Science, 43(9): 3200-3217. doi: 10.3799/dqkx.2018.559

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Magma Mixing in Halagatu Granitic Batholith from Eastern Part of the East Kunlun Orogenic Belt: Constraints from Lithology and Mineralogy

doi: 10.3799/dqkx.2018.559

1.
Key Laboratory of Western Mineral Resources and Geological Engineering, Ministry of Education; School of Earth Science and Resources, Chang'an University, Xi'an 710054, China
2.
School of Civil Engineering, Nanyang Institute of Technology, Nanyang 473000, China

Received Date: 2018-02-13
Publish Date: 2018-09-15

Abstract

Abstract

Magma mixing events occurred widely and fiercely in Halagatu granitic batholith in eastern part of the East Kunlun orogenic belt, one of the ideal natural labs for magma mixing and mingling studies. We study through electron microprobe (EPMA) the lithology, petrography and mineral chemistry from the granitic batholith. The results reveal that plagioclases in the host rocks and those in the xenocrystals in MMEs have similar mineral features of anorthite-albite component value (An value). And most plagioclases in matrix of MMEs have core-rim structures with an An value discontinuity. An values of the light-colored matrix plagioclase in some MMEs are similar to those with core-rim structures. The plagioclases in gabbro diorite have a higher An value. The crystallization temperature, pressure and oxygen fugacity of the hornblendes of the host rocks are similar to those of the hornblende xenocrystals in MMEs. The crystallization temperature and pressure of the matrix hornblende in the MMEs are lower than those in the host rocks, and the oxygen fugacity is slightly higher than that in the host rocks. The hornblendes in gabbro diorite have the highest crystallization temperature and pressure and the lowest oxygen fugacity. The compositions of the plagioclase and hornblende in the host rocks of the Hatugou section and Defusheng section are different. Intermittent magma intrusions and crystallizations, together with their evolution resulted in differences in composition, physical and chemical features varying with places. The mafic magma stayed in deep the Crust with lower oxygen fugacity, providing a condition of high pressure and low oxygen fugacity for hornblende crystallization and high An value for plagioclases. With the injection of mafic magma into the host rocks, due to environmental changes, plagioclases are subject to erosion. The temperature, pressure and water saturation reduced, whilst oxygen fugacity increased because of magma intrusion and physical and chemical differences for the two magmas. Thus the residual magma in MMEs crystallized quickly to form plagioclases with core-rim structures and uniformly light color, and hornblendes with non-crystal shape and high value of oxygen fugacity.
- East Kunlun orogenic belt,
- Halagatu granitic batholith,
- mineral chemistry,
- magma evolution,
- magma mixing,
- geochemistry

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References(100)

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