罗布莎豆荚状铬铁矿床中刚玉的含Ti矿物包裹体特征

徐向珍; 杨经绥; 熊发挥; 郭国林

doi:10.3799/dqkx.2018.706

Volume 43 Issue 4

Apr. 2018

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Article Navigation > Earth Science > 2018 > 43(4): 1025-1037

Xu Xiangzhen, Yang Jingsui, Xiong Fahui, Guo Guolin, 2018. Characteristics of Titanium-Bearing Inclusions Found in Corundum of Luobusa Podiform Chromitite, Tibet. Earth Science, 43(4): 1025-1037. doi: 10.3799/dqkx.2018.706

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Xu Xiangzhen, Yang Jingsui, Xiong Fahui, Guo Guolin, 2018. Characteristics of Titanium-Bearing Inclusions Found in Corundum of Luobusa Podiform Chromitite, Tibet. Earth Science, 43(4): 1025-1037. doi: 10.3799/dqkx.2018.706

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Characteristics of Titanium-Bearing Inclusions Found in Corundum of Luobusa Podiform Chromitite, Tibet

doi: 10.3799/dqkx.2018.706

1.
Center for Advanced Research on Mantle(CARMA), Key Laboratory of Deep-Earth Dynamics of Ministry of Land and Resources, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
2.
State Key Laboratory Breeding Base of Nuclear Resources and Environment, East China Institute of Technology, Nanchang 330013, China

Received Date: 2017-12-18
Publish Date: 2018-04-15

Abstract

Abstract

The titanium-bearing alloy and titanium-bearing oxide inclusions in corundum collected from Luobusa podiform chromitite in Tibet are studied. The EDS and EPMA analyses show that the Ti-N alloys are rounded or forming a quincunx with the size of 17 μm×35 μm; the Ti-B alloys are long columnar in size of 10 μm×58 μm; the authigenic and exnotopic Ti-C alloys are 40 μm×50 μm; the Ti-Si-P and Ti-Si-Fe alloys occur as highly heterogeneous melt in the corundum and the Ti-Al-Zr oxides are pretty pure in composition. Considering the unusual ultra-high pressure mantle mineral groups like diamond and moissanite recovered from the Luobusa chromitite, it is suggested that the corundum and its special mineral inclusions might form at the high-pressure deep mantle environment.
- mineral inclusion,
- corundum,
- chromitite,
- Luobusa,
- Tibet

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References(84)

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