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《BULLETIN OF MINERALOGY PETROLOGY AND GEOCHEMISTRY》 2000-02
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Ore-Formation of Basin Fluids in the Northern Margin of North China Craton-Case Studies

CHEN Xu rui 1 , LIU Jian ming 1 , YANG Si dao 2, ZHANG An li 3 , ZENG Heng rong 2[WT9.5BX](1.Institute of Geology and Geophysics,CAS, Beijing 100101, China;2.Dajing Silrer copper Mining Company, Linxi, Neimeng, 025250, China; 3. 514 Geologic  
WT5BZ]There occur ore deposits formed by basin fluids in the northern margin of North China Craton (including its northern crustal growth zone during Paleozoic), and the ore formation always related with rifting basins, just like the situation of Yangtze Craton in South China. According to evolutional dynamics characteristics of sedimentary basin , there are two metallogenic provinces in connection with basin fluid ore formation in the northern margin of North China Craton:1) Proterozoic Au polymetallic province in the northern part of the craton, where sedex type Pb Zn polymetal deposits and sediment hosted micro disseminated gold (SMG) deposits were formed by basin fluids in Proterozoic rifting basins;2) Paleozoic Sn polymetallic province in the northern accretionary zones of the craton, where Pb Zn and Sn polymetallic deposits were formed in Paleozoic basins with extensional tectonic background.
【Fund】: 中科院重大项目!(KZ95 1 B1 40 4);; 科技部攀登预选项目!( 95 预 3 9)资助
【CateGory Index】: P544.4
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