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- W2371141974 abstract "The Suolajier Cu-Mo deposit which was newly discovered in Qimantage in western part of eastern Kunlun Mountains,displays a geological feature of metals-bearing hydrotherm invading into broken skarn and marble.This paper summarizes its mineralization system through a mineralization process that Kunbei post-arc rift happened in early Paleozoic(Ordovician-Silurian),Tanjianshan formation from hot water sediment as the original mineral sources,the magma in Indosinian Epoch provided strong heat source and hydrotherm to reshape the skarn layer,metallic elements were enriched in broken skarn and marble into mineralization.This paper also discusses how to develop the deposit and studies the feasibility to establishing a mining town in Qinghua." @default.
- W2371141974 created "2016-06-24" @default.
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- W2371141974 date "2010-01-01" @default.
- W2371141974 modified "2023-09-22" @default.
- W2371141974 title "MINERALIZATION SYSTEM AND DEVELOPMENT CONDITIONS OF SUOLAJIER CU-MO DEPOSIT IN EASTERN KUNLUN" @default.
- W2371141974 hasPublicationYear "2010" @default.
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