Abstract There are widelydistributed sedimentary rocks in Guizhou, especially in central Guizhou. In
western Guizhou, large areas of Permian basalts are exposed at surface together with sporadic diabase, and
in the southeastern part of eastern Guizhou, extensivelyexposed metamorphic rocks are seen with sporadic
basicultrabasic rocks in between. Gigantic Xuefengian granite batholiths occur from the GuizhouGuangxi
border area to Guangxi. There locally exist granites of Wuling period in northeastern Guizhou, forming a
mysterious distribution map of strata and intrusive bodies on the YunnanGuizhou plateau. Large amounts of
Al, P, Au, PbZn, Hg and coal deposits have already been discovered, forming one of the important ore
prospect areas in Southwest China. Nevertheless, intermediateacid intrusive bodies related to mesothermal
epithermal ore resources are hardly seen at surface in Guizhou Province, with only very few bodies
exposed in Fanjingshan (Wulingyuan) area.
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