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- W2351534401 abstract "Through the study on the fine granite,the underground-explosive breccia and the isotope feature of the Niujuan silver(gold) deposit,this article suggests that the underground-explosive breccia(sub-lava) is formed by the partial remelting of basal rocks.The metallogenic material is from the remelting magma of the lower crust-upper mantle.The metallogenic hydrotherm is gas-rich liquid formed by differentiation of remelting magma.Ascending with or after the sub-lava,the liquid forms deposit in crushed zone after many times of underground exploding.As a vein,the silver orebody occurred in the crushed zone of coarse-grained granite.The ore-bearing rock is underground explosive breccias.The magma material forms both gravel and cement.The alteration is epithermal and mesothermal.The deposit should be epithermal and mesothermal deposit formed by underground exploding of ore-bearing tuff." @default.
- W2351534401 created "2016-06-24" @default.
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- W2351534401 date "2010-01-01" @default.
- W2351534401 modified "2023-09-23" @default.
- W2351534401 title "Study on the Genesis of the Niujuan Silver(Gold) Deposit in Hebei Province" @default.
- W2351534401 hasPublicationYear "2010" @default.
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