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- W2356950467 abstract "This paper presents the recent research results on the occurrence,distribution,geological and geochemical characteristics,genesis and metallogenesis of alkaline complexes in China mainland. The petrographic and isotopic characteristics indicate that silica-undersaturated alkaline complex is mostly the product of original magma emplacement,which mainly comes from low-degree partial melting mantle. However,silica-saturated or silica-supersaturated alkaline complex is mostly the product of deep source magma contaminated by continental crust. Low-degree partial melt of mantle source led to the enrichment of rare earth elements,large ion lithophile elements and other incompatible elements,while the volatile material enriched in the same time constitutes mineralizer,which has an important controlling role in mineralization. Deep faults control the output of alkaline complex,accompanied by significant geological events in geological history. Alkaline complex zones controlled by deep faults in China mainland include nine major alkaline complex zones,such as the Tancheng-Lujiang alkaline complex zone,Panxi alkaline complex zone and Ailaoshan-Jinsha River alkaline complex zone." @default.
- W2356950467 created "2016-06-24" @default.
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- W2356950467 date "2015-01-01" @default.
- W2356950467 modified "2023-09-24" @default.
- W2356950467 title "Genesis and Metallogenesis of Alkaline Complexes in China Mainland" @default.
- W2356950467 hasPublicationYear "2015" @default.
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