Abstract:
In the middle part of the Xuefengshan mountain exist many types of gold deposits,of which a new type-a strata bound gold deposits often widespread and of high grade has been recently discovered.The gold deposit is closely associated with the feldspathic quartz gray-wacke of the Zhuanqiangwan Formation of the Furongxi Group (Pt
fz) and the pebble-bearing feldspathic quartz gray-wacke of the Sinian Changtan Formation(Z
c)."T" shaped high grad gold ores usually occur in the confluence of various types of alteration or where the NW-trending structures join the NE-trending structures.