Petrogenesis and metallogenesis of the Yaxi gabbroic intrusion associated with Fe-Ti-V-P ores in eastern Tianshan, NW China
Ore Geology Reviews(2019)
摘要
•The Yaxi gabbro emplaced at 308.7 ± 1.4 Ma, possibly during the postcollisional stage.•The Yaxi gabbro originated from partial melting of enriched lithospheric mantle.•The formation of the Yaxi deposit benefited from fractional crystallization.
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关键词
Yaxi Fe-Ti-V-P deposit,Zircon U-Pb age,Mafic intrusion,Eastern Tianshan,Postcollisional extension
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