Genesis of the Large-Scale Kamado Magnesite Deposit on the Tibetan Plateau

Genesis of the Large-Scale Kamado Magnesite Deposit on the Tibetan Plateau

Lacustrine strata-bound magnesite deposits associated with Alpine-type ultramafic rocks are hydrothermal in origin. The magnesite ores of the Kamado deposit are unconformably underlain by mid-Jurassic marine carbonate and ultramafic rocks of the Bangong-Nujiang ophiolite suite and are in fault conta...

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Bibliographic Details
Main Authors: Xuhui Yu, Guyue Hu, Yuchuan Chen, Ying Xu, Han Chen, Denghong Wang, Fan Huang, Shuisheng You, Haiyong Liu, Liang He, Yubin Li
Format: Article
Language:English
Published: MDPI AG 2023-12-01
Series:Minerals
Subjects:
lacustrine hydrothermal-sedimentary mineralization
ultramafic rocks
suture zone
geochemistry
carbon isotopes
oxygen isotopes
Online Access:https://www.mdpi.com/2075-163X/14/1/45

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https://www.mdpi.com/2075-163X/14/1/45

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