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- W2374805105 abstract "According to regional metallogenic theory,East Qinling structural belt can be divided into the southern margin of North China paleo-continent,orogenic belts of North Qinling and South Qinling,and the fourth tectonic unit of the Yangtze paleo-continent.The South and North Qinling orogenic belts are bound by the Shangdan suture-fault zone,forming the boundary of North China paleo-continent and South China paleo-continent.Fractures and Yanshanian magmatic rocks are well developed within the East Qinling structural belt.The study area is located at the margin of the block,with dual mesa sedimentary structure composed of basement and cap-rocks.The basement consists of Archean Taihua Group metamorphic rock and Xiong'er Group volcanic rocks and Yanshanian magmatic rocks,which constitutes ore source rocks in this area.Ore source rocks are characterized by depletion in Cu and enrichment in W,Mo,Zn,Pb,Au and Ag in the cap-rocks.Mineral resources are rich in this area,and dominated by hyrdothermal genetic Mo-Au polymetallic deposits.Based on the genesis of ore-forming fluid and other geological actions,three metallogenic systems are classified,including magmatic hydrothermal metallogenic Mo-Au polymetallic deposits,volcanic hydrothermal metallogenic system and tectonic hydrothermal metallogenic system.They are correspondingly related to early Yanshannian hydrothermal activities,Xiong'ernian volcanic hydrothermal and Mesozoic tectonic hydrothermal activities.Meanwhile,the key metallogenic areas within the study area are predicted based on the analysis of regional tectonic natures of the three tectonic activities." @default.
- W2374805105 created "2016-06-24" @default.
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- W2374805105 date "2010-01-01" @default.
- W2374805105 modified "2023-09-26" @default.
- W2374805105 title "Metallogenic System and Prediction of Mo-Au Polymetallic Deposits in East Qinling" @default.
- W2374805105 hasPublicationYear "2010" @default.
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