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- W2379938909 abstract "Dalong W-Mo deposit in Tibet locates at the northern side of eastern section of Gangdese metallogenic belt which is controlled by Dalong regional fault zone.The ore-bodies occur in silicified garnet slates and diopside Skarn in veined,slabby and vesiculate shapes.The average grade of WO3 is 0.212%,while that of Mo is 0.091%and that of Zn is 3.10%.The fluid inclusion thermometry shows that the formational temperature of W-Mo is 320℃ while that of Cu-Zn is 200℃.The sulfur isotopeδ34S is determined in the range of3.5‰~5.5‰ which indicates that the metallogenic materials are deep seated source.According to the Re-Os dating of molybdenite,its model age is within the range of 63.2~68.1Ma and its mineralization period is early Himalayan stage.The mineralization of W-Mo is primarily related to skarnization formed from emplacement of biotite granodiorite." @default.
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- W2379938909 date "2014-01-01" @default.
- W2379938909 modified "2023-09-27" @default.
- W2379938909 title "Geological characteristics and mineralization environment of Dalong W-Mo deposit in Tibet" @default.
- W2379938909 hasPublicationYear "2014" @default.
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