东昆仑香加花岗质岩体中镁铁质包体成因:岩相学及地球化学证据

秦拯纬; 马昌前; 付建明; 卢友月; 史洪峰; 熊富浩

doi:10.3799/dqkx.2018.549

Volume 43 Issue 7

Jul. 2018

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Qin Zhengwei, Ma Changqian, Fu Jianming, Lu Youyue, Shi Hongfeng, Xiong Fuhao, 2018. The Origin of Mafic Enclaves in Xiangjia Granitic Pluton of East Kunlun Orogenic Belt: Evidence from Petrography and Geochemistry. Earth Science, 43(7): 2420-2437. doi: 10.3799/dqkx.2018.549

Citation:

Qin Zhengwei, Ma Changqian, Fu Jianming, Lu Youyue, Shi Hongfeng, Xiong Fuhao, 2018. The Origin of Mafic Enclaves in Xiangjia Granitic Pluton of East Kunlun Orogenic Belt: Evidence from Petrography and Geochemistry. Earth Science, 43(7): 2420-2437. doi: 10.3799/dqkx.2018.549

Citation:

Qin Zhengwei, Ma Changqian, Fu Jianming, Lu Youyue, Shi Hongfeng, Xiong Fuhao, 2018. The Origin of Mafic Enclaves in Xiangjia Granitic Pluton of East Kunlun Orogenic Belt: Evidence from Petrography and Geochemistry. Earth Science, 43(7): 2420-2437. doi: 10.3799/dqkx.2018.549

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The Origin of Mafic Enclaves in Xiangjia Granitic Pluton of East Kunlun Orogenic Belt: Evidence from Petrography and Geochemistry

doi: 10.3799/dqkx.2018.549

1.
Wuhan Center of China Geological Survey, Wuhan 430205, China
2.
Research Center of Granitic Diagenesis and Mineralization, China Geological Survey, Wuhan 430205, China
3.
Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China
4.
Nanjing Center of Geological Survey, China Geological Survey, Nanjing 210016, China
5.
Faculty of Earth Sciences, Chengdu University of Technology, Chengdu 610059, China

Received Date: 2017-09-28
Publish Date: 2018-07-15

Abstract

Abstract

The East Kunlun orogenic belt is characterized by widespread Early-Middle Triassic Epoch granitic rocks with a large proportion of mafic enclaves therein, however, there is still lack of petrography and mineralogy studies on the Mafic enclaves with different textures. In this paper, a systematic petrography and mineral chemistry study has been carried out for the representative Xiangjia granite pluton as well as the enclosed Mafic enclaves, which have clarified the processes of crust-mantle interaction in East Kunlun area. Studies on petrography have shown that the mafic enclaves have some disequilibrium textures and some phenomenon point to rapid crystallization, such as needle-like apatite, needle-like amphibole and augen-shaped quartz, all of which suggest the possible of magma mixing process, and the enclave with ophitic-gabbro texture likely to be the basic end-member. In addition, multi-stage growing of feldspar indicates there might be multi-mixing process. Whole rock geochemistry shows that the mafic enclaves have lower Mg^# and higher Fe^# values relative to their host rocks (Mg^#:0.39-0.56, Fe^#:0.44-0.62). Electron microprobe investigation shows that enclaves have two kinds of amphiboles, one kind in mafic enclaves (TiO₂:2.1%-2.9%, SiO₂:41.75%-44.49%) crystallized from mantle-derived basic magma in the early stage, while the other kind (TiO₂:1.0%-1.8%, SiO₂:42.49%-48.10%) probably crystallized from the mixed magma in the shallow crust level. Some biotites (MgO:9.78%-11.53%, Mg^#:0.462-0.541) are similar to biotites crystallizing in the mantle-derived magma. The rhythmic zoning and geochemistry contents of Plagioclases show that they may have suffered the process of magma mixing. Calculated results by geobarameter indicate that the mantle-derived basic magma crystallized under 5×10⁸ bar, i.e. about 18 km depth, producing the high-Ti amphiboles, and then mixed with the acid magma. The mixed magma emplaced to upper crust, maybe at 2.5×10⁸ bar, i.e. about 8km depth, producing the Low-Ti amphiboles. All these features above show that the East Kunlun orogenic belt might have experienced crust-mantle interaction repeatly during the Triassic Epoch, and the injection of mantle magma played an important role in the crustal growth and crust anatexis. The wide crust-mantle interaction may be the response to the slab break-off of Animaqing Ocean during the Triassic Period.
- East Kunlun orogenic belt,
- mafic enclaves,
- granite,
- geochemistry,
- multi-mixing

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References(75)

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