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《Journal of Jiling University (Earth Science Edition)》 1988-03
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LEAD ISOTOPE COMPOSITION OF GOLD DEPOSITS, NORTH-WESTERN JIAODONG SHANDONG, AND ITS GEOLOGICAL SIGNIFICANCE

Wang Yi wenI ilin Research Diointon of Geology and Vincral Reources China Nonferrons Metals Industrial Company)  
The metnsomatie-anmcctitic granitoid related gold(and silver)deposits, the Meso-zoic voleanics relaied Pb-Zn deposits and the metasomatic-anatectie granitoid itself possess lead isotope compositions similar to the mecamorphic roots of Jiaodong Group.The leads are all of multi-stage leads derived from an Th/U deplated source.The points plotted on the 207Pb/204Pb-203Pb/204Pb diagram distribute in a linear array (the 2nd-stage isochrone or the mixing line) , According to the slope(0.2601)of the line and many K/Ar, U/Pb, Rb./Sr, 30Ar/40Ar age data, following conclusions were reachcd:t1 = 3.2Ga. t2 = 0.15Ga, μλ = 7.07 - 8.17, W1-29 .16 - 35.80, Th/U-3.97-4.52.Comparing these with the values of the Earth and the Jiaodong Group, the clculated parameters show that the leaks of the Au(Ag), Pb-Zn deposits and me-taasomatic-anatexite granitoid were derived from a mobilized lower crust and the different types of gold deposits in Jiaodong district were formed in the process of plate subduction in the Mesozoic and can be called as hydrothermal deposits related to metasomatic-anatectic granitoid.
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