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《Geotectonica Et Metallogenia》 1985-04
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A LEAD ISOTOPE STUDY OF THE IRONCOPPER POLYMETALLIC ORE ZONE IN THE MIDDLE LOWER YANTZE RIVER AND ITS GEOTECTONIC AND METALLO GENIC SIGNIFICANCE

YE Jingren (Changsha Institute of Geotectonic, Academia Sinica)  
The whole-rock lead isotope of the Mesozoic calc-alkaline magmatic rock and Carboniferous-Permian limestone in this region has been studied. The lead isotope of galena from Pb-Zn deposits and occurrences of various genetic types has also been studied, and further the evolution and metallogeny of lead in different geotectonic stages disussed. On this basis, the paper points out that the calc-alkaline magmatic rock is the product formed by contamination of mantle derived magma with continental crust consolidated 1600m.y, ago. Ore-forming material of the Pb—Zn deposits and occurrences located in the magmatic rock and along the contact zone was derived directly from post-magmatic hydrothermal solution, while ore-forming material of strata-bound Pb—Zn deposits and occurrences located far away from the contact zone was derived by remobilization in the diwa(geodepre-ssion) stage from the ancient platform sedimentary cover formed 340—900m.y.ago. The Carboniferous-Permian limestone is only an important ore-forming country rock, but not a source bed.
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