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- W2362488497 abstract "The Dajing tin-polymetallic deposit, Inner Mongolia, is a hydrothermal vein-type deposit related to volcanic and sub-volcanic rocks. The ore-forming elements are complicated, which have oxyphile (Tin) and chalcophile (Cu, Pb, Zn, Ag) ore-forming elements combination. Dykes in this mining area well development. They can be divided into two categories: felsitic rock and dacite porphyry rock. In the felsitic rock, phenocrysts are not developed, silicified and sericitization strongly, and the features of loss of Eu is significant, all these are have relationship with the tin in early stages; In the dacite porphyry rock, phenocrysts are developed, pyritization strongly, and the features of loss of Eu is not obvious, formed andesitic porphyry-diorite porphyrite-dacite porphyry veins combination, all these have relationship with Cu, Pb, Zn mineralization. Two sets of dikes represent magma-mineralization system at different stages and the same (near) structural positions has successively superimposed mineralization, which formed the complex ore-forming elements combination in Dajing deposit. Dykes and their alteration characteristic are the important prospecting criteria in this area." @default.
- W2362488497 created "2016-06-24" @default.
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- W2362488497 date "2011-01-01" @default.
- W2362488497 modified "2023-09-23" @default.
- W2362488497 title "The Mineralization and Prospecting Significance of Dykes of Dajing Tin-Polymetallic Deposit, Inner Mongolia" @default.
- W2362488497 hasPublicationYear "2011" @default.
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