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- W2385286711 abstract "The Lashuixia Ni-Cu sulfide deposit is an important Cu-Ni-rich deposit in Qinhai Province. Geochemical studies of the basic complex closely associated with the deposit show that it is characterized by low Ti, depletion of Nb or Ta, and enrichment of LREE and large lithosphile elements. Combined with their isotope geochemistry, it is concluded that the formation of the basic complex is related to the conversion from subduction to collision between the Qilian Mountains and their adjacent areas at 460~440 Ma. The magma was derived from the enriched lithospheric mantle, contaminated by crustal materials within the high-level magma chamber. This process led to the increasing amount of Si, and triggered the immiscibility between the sulfides-rich liquid and the silicate-rich liquid." @default.
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- W2385286711 date "2012-01-01" @default.
- W2385286711 modified "2023-09-28" @default.
- W2385286711 title "Geochemical Characteristics of the Lashuixia Basic Complex in Qinhai Province and Its Constraints on Genesis of the Deposit" @default.
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