藏南拿日雍措片麻岩穹窿淡色花岗岩稀有金属的富集

高利娥; 曾令森; 胡古月; 高家昊; 赵令浩; 王亚莹

doi:10.3799/dqkx.2018.390

Volume 44 Issue 6

Jun. 2019

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Article Navigation > Earth Science > 2019 > 44(6): 1860-1875

Gao Li'e, Zeng Lingsen, Hu Guyue, Gao Jiahao, Zhao Linghao, Wang Yaying, 2019. Rare Metal Enrichment in Leucogranite within Nariyongcuo Gneiss Dome, South Tibet. Earth Science, 44(6): 1860-1875. doi: 10.3799/dqkx.2018.390

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Gao Li'e, Zeng Lingsen, Hu Guyue, Gao Jiahao, Zhao Linghao, Wang Yaying, 2019. Rare Metal Enrichment in Leucogranite within Nariyongcuo Gneiss Dome, South Tibet. Earth Science, 44(6): 1860-1875. doi: 10.3799/dqkx.2018.390

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Rare Metal Enrichment in Leucogranite within Nariyongcuo Gneiss Dome, South Tibet

doi: 10.3799/dqkx.2018.390

1.
Key Laboratory of Deep-Earth Dynamics, Ministry of Natural Resources, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
2.
Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China
3.
National Research Center for Geoanalysis, Chinese Academy of Geological Sciences, Beijing 100037, China

Received Date: 2018-08-17
Publish Date: 2019-06-15

Abstract

Abstract

The Nariyongcuo gneiss dome, located to eastern Tethyan Himalaya, consists of many types of granites, containing twomica granite, foliated leucogranites, garnet-bearing leucogranite, garnet-bearing pegmatite, and beryl-bearing pegmatite. All the Nariyongcuo leucogranites are evolved granites and resulted from various degrees of collective fractional crystallization of plagioclase, zircon, monazite, apatite and Ti-rich mineral phases. Comparing with Victorinox value of granites, these granites are enriched in rare metal elements of Bi, Cs, Li, Sn, Be, Pb, B, W, Ta, but relatively depleted in Nb. In addition, the wall rocks are also enriched in rare metal elements. Whole rock geochemical data imply that fractional crystallization and hydrothermal metasomatism resulted in rare metal mineralization within the Nariyongcuo gneiss dome. In the Himalayan belt, high evolved granites are widely distributed, and commonly contain rare metal-bearing minerals (niobite, tapiolite, cassiterite, beryl), suggesting that the Himalaya belt could be another new important target for the exploration of race metal deposits.
- South Tibet,
- Nariyongcuo gneiss dome,
- leucogranite,
- rare metals,
- beryl,
- petrology

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References

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Rare Metal Enrichment in Leucogranite within Nariyongcuo Gneiss Dome, South Tibet

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