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《Journal of Jiling University (Earth Science Edition)》 1989-03
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THE GENESIS OF GOLD DEPOSIT IN SOUTH LONGWANGMIAO SYN-DUCTILE SHEAR BELT IN ARCHEAN GREENSTONE, NORTH LIAONING, CHINA

Dai Shibing  
South Longwangmiao gold deposit in Liaoning Province occurred in the meta-felsic rock unit in Liaobei Archean greenstone belt.Two different ore bodies were controlled by the deepseated ductile shear zone of epidote-amphibolite facies.There are discoverable alterations near ore bodies.Gold is mostly found in pyrite and fills fissues. The fineness of gold is 946. The correlation between rare elements and ore shows that gold was derived from the greenstone. Sulphur and lead isotopes indicate that sulphur and lead were also derived from the greenstone.Hydrogen and oxygen isotopes of inclusions in veinlike quartz show that water is of metamor-phic origin.Consequently the gold deposit is of matamorphic hydrothermal origin and is synductile shearing in Archean, which is the oldest one found in China so far.
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