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《Resources Survey & Environment》 2010-01
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Mineralization significance of Zhejiang-Fujian rift-valley belt

WANG Cheng-liang(No.7 Geological Prospecting Party of Zhejiang province,Lishui 323000,China)  
The Zhejiang-Fujian rift-valley belt is an important belt of Au,Ag,Cu,Pb,Zn,Mo metallic mineral resources and fluorite,kaolin and other nonmetallic mineral resources.The typical mineral deposits include Zhilintou Au-Ag deposit,Meixian type massive sulfide polymetallic deposit,Yingkeng porphyry Mo deposit, Hushang and Wuyi fluorite ore-fields and others.The activity of the rift-valley belt had two cycles,the first one,being in correspondence with disintegrating of Rodinia supercontinent,started from Later Proterozoic and closed in Caledonian period,its representative stratigraphic sign is occurrence of Middle Proterozoic strata.The second one started from Early Yanshanian period and ended in Later Yanshanian period,the typical stratigraphic sign is occurrence of Lower Jurassic Fengping Formation and sedimentary strata of Cretaceous faulted basins.The first cycle is correspondent with geological processes including regional metamorphism,migmatization,ductile shearing and magma intrusion.The second cycle is correspondent with geological processes including large-scale volcanic exhalation,magma intrusion and formation of faulted basins.During the first cycle in the rift-valley environment,the preliminary mineralization enrichments of Zhilintou type Au-Ag deposit and Meixian type sulfide Pb-Zn polymetallic deposit were occurred;while during the late stage of the second cycle,the large-scale volcanic hydrothermal mineralizations caused further mineralization enrichments which overlapped on the former deposits,and magma intrusion caused to form a series of porphyry Cu-Mo deposits as well as nonmetallic,fluorite mineralization belts with distinctive features in Zhejiang-Fujian region.
【CateGory Index】: P611
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