吉林夹皮沟金矿稳定同位素地质及找矿方向

吉林夹皮沟金矿床成因，多年来一直存在变质热液和岩浆热液之争。在金矿带北侧海西期花岗岩内和南侧白山镇一带变质岩地区进行外围找矿始终没有突破性进展。在前人研究基础上，通过一些补测工作对夹皮沟金矿稳定同位素地质给予新的认识。Ｓ和Ｃ、Ｈ、Ｏ流体主要来自地幔，部分Ｓ和Ｓｉ、Ｐｂ、Ａｕ主要来自花岗岩和古老变质层状岩系，成矿远景区应重点选定在夹皮沟—大砬子深大断裂两侧中生代脉岩体附近。

THE STABLE ISOTOPIC GEOLOGY AND EXPLORATION DIRECTION OF THE JIAPIGOU GOLD ORE DEPOSIT, JILIN PROVINCE

There has long been controversy on the genesis of the Jiapigou gold ore deposit, metamorphic hydrothermal or magmatic hydrothermal. Therefore, there is no great progress in the gold exploration in the Hercynian granite to the north and in the metamorphic terrene near Baishanzhen to the south. Further work on the stable isotope analysis is conducted by the authors. It is proposed that the S,C,H and O bearing fluids are derived from the mantle and some of the S,Si,Pb and Au from the granite and metamorphic layered sequence. The metallogenic prognosis province is expected to be near the mesozoic dykes near the Jiapigou Dalazi deep fault.