西藏错那洞电气石花岗岩中电气石化学组成、硼同位素特征及意义

代作文; 李光明; 丁俊; 张林奎; 曹华文; 张志; 梁维

doi:10.3799/dqkx.2019.043

Volume 44 Issue 6

Jun. 2019

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Dai Zuowen, Li Guangming, Ding Jun, Zhang Linkui, Cao Huawen, Zhang Zhi, Liang Wei, 2019. Chemical and Boron Isotopic Composition, and Significance of Tourmaline from the Cuonadong Tourmaline Granite, Tibet. Earth Science, 44(6): 1849-1859. doi: 10.3799/dqkx.2019.043

Citation:

Dai Zuowen, Li Guangming, Ding Jun, Zhang Linkui, Cao Huawen, Zhang Zhi, Liang Wei, 2019. Chemical and Boron Isotopic Composition, and Significance of Tourmaline from the Cuonadong Tourmaline Granite, Tibet. Earth Science, 44(6): 1849-1859. doi: 10.3799/dqkx.2019.043

Citation:

Dai Zuowen, Li Guangming, Ding Jun, Zhang Linkui, Cao Huawen, Zhang Zhi, Liang Wei, 2019. Chemical and Boron Isotopic Composition, and Significance of Tourmaline from the Cuonadong Tourmaline Granite, Tibet. Earth Science, 44(6): 1849-1859. doi: 10.3799/dqkx.2019.043

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Chemical and Boron Isotopic Composition, and Significance of Tourmaline from the Cuonadong Tourmaline Granite, Tibet

doi: 10.3799/dqkx.2019.043

Dai Zuowen^{1,2
,
,},
Li Guangming^{2
,
,
,},
Ding Jun²,
Zhang Linkui²,
Cao Huawen²,
Zhang Zhi²,
Liang Wei²

1.
College of Earth Sciences, Chengdu University of Technology, Chengdu 610059, China
2.
Chengdu Center, China Geological Survey, Chengdu 610081, China

Received Date: 2018-07-20
Publish Date: 2019-06-15

Abstract

Abstract

In order to further constrain the source of the Cuonadong tourmaline granite, Tibet, morphology, chemical and isotopic composition of the tourmaline were studied by means of the microscope, electron probe, laser ablation multi-collector inductively coupled plasma mass spectrometer. The results indicate that the tourmaline from the Cuonadong tourmaline granite belongs to alkali group, and is schorl, which crystallized from boron-rich melts, indicating no obvious boron isotope fractionation between tourmaline and the melts has occurred.δ¹¹B values of the tourmaline from the Cuonadong tourmaline granite range from-6.91‰ to-9.17‰, which are close to the average δ¹¹B value (-10‰ ±3‰) of the continental crust, implying that the Cuonadong tourmaline granite was derived from partial melting of metasedimentay rock. However, δ¹¹B values of the tourmaline from the Cuonadong tourmaline granite is much higher relative to granites derived from metasedimentary rock, and similar to δ¹¹B values of Yardoi leucogranite reported by previous research, which was originated from garnet-amphibolite. Thus, besides metasedimentary rock, there was probably a small amount of garnet-amphibolite present in the source region of the the Cuonadong tourmaline granite.
- Tibet,
- Himalaya,
- Cuonadong,
- leucogranite,
- tourmaline,
- Boron isotope,
- petrology,
- crust source

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References(49)

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Chemical and Boron Isotopic Composition, and Significance of Tourmaline from the Cuonadong Tourmaline Granite, Tibet

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