Under hygrothermal climate, a series of physicochemical changes take place on huebnerite-scheelite deposit,containing polymetallic sulphi-des and slich a deposit forms a secondary tungsten deposit.
在温湿气候条件下,含多化物的钨锰-白钨矿矿床会产主一系列的物理、化学化,形成次生富集钨矿床。
Under hygrothermal climate, a series of physicochemical changes take place on huebnerite-scheelite deposit,containing polymetallic sulphi-des and slich a deposit forms a secondary tungsten deposit.
在温湿气候条件下,含多化物的钨锰-白钨矿矿床会产主一系列的物理、化学化,形成次生富集钨矿床。
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