THE FEATURE OF QINGGANGPING GOLD DEPOSIT AND STUDY ON THE STABIE ISOTOPE, XIONGERSHAN AREA,WESTERN HENAN PROVINCE

Qinggangping deposit is a low-angle altered fractural rock type gold deposit. It is low-angle, thin,high grade and long extending. The study on stable isotopes suggests the metallo-genic material derived from Huashan granite. As other gold deposits in Xiongershan area the deposit is formed by Yanshannian granite. There are metallogenic conditions for middle-large scale gold deposits.