Modern Mining ›› 2020, Vol. 36 ›› Issue (06): 30-.
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Jin Xin1Yu Can 2
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Abstract: Dahongshan Copper Deposit is a volcanic exhalationtransport and depositionmetamorphic reformation type deposit,which characterized by rich mineralization and complicated genesis.Based on systematic collection of geological data of Dahongshan mining area,the occurrence and enrichment mechanism of goldsilver mineralization is obtained by combined with the field geological surveying and test results.The study results show that:①the independent goldsilver mineral are mainly occurred in chalcopyrite and pyrite;②the submarine volcanic exhalationsedimentation establish foundation for goldsilver mineralizaiton,in addition,the foldsilver mineralization is mainly occurred in third lithologic member of Manganghe Formation;③the significant positive correlation between the goldsilver mineralization and copperiron mineralization is presented,which have most mineralization internsity among I2,Ib and I3 oresection;④the goldsilver mineralization has the characteristic of stratabound,and the ore evolution strictly controlled by volcanic activity and lithogacies paleogeography,the formation lithology,wallrock alteration,geophysical characteristics can be regarded as the prospecting criteria for Dahongshan goldsilver mineralization.
Jin Xin Yu Can. Mineralization Enrichment Regularity and Ore Prospecting of Associated Goldsilver for Dahongshan Ironcopper Deposit[J]. Modern Mining, 2020, 36(06): 30-.
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