Jinman vein copper deposit in western Yunnan occurs in a salt-bearing red e
lastic rock formation composed of sandstone, siltstone and shale. Wood text
ure is considerably developed in the ores. The metallic minerals making up
the wood textures mainly include pyrite, chalcopyrite and bornite, Studies
on the samples and examination of their micrographs and electron micrograph
s have confirmed that they belong to xenoxylon, reflecting that the ore-hos
ting rock series is the product of sedimentation in the terrestrial environ
ment. Organic geochemistry and sulfur and carbon isotopic composition data
indicate that the formation of the deposit is substantially related with un
derground hot brines and biological processes.