The volcanic exhalative rocks of Baiziyan Formation in Wutai greenstone belt is composed of basic mid acid volcanic rocks, tuffs and tourmaline and flogopite bearing quartz marble, in which gold deposit occurs.

Dongyaozhuang gold deposits is in Wutaishan greenstone belt.

Study on mineralogy, petrology, mineral deposit geology and determining prospecting criteria of such type gold deposit have great significance to prospecting they in Wutaishan greenstone belt.

In Wangjiahui granitic pluton of Wutai granite-greenstone belt, gneissiosity and lineation structures were formed in the late stage of magmatic emplacement, when the pluton was a Bingham body.

The paper has introduced the structural character of Hutuo group and Wutai rock group-the terranes are parallel and accordant with each other,and analyzed why the stratums metamorphic grade of Hutuo group and Wutai rock group is accordant.

show that the climax value of Hengshan complex’s (2520 Ma) is 20Ma less than Wutai complex’s (2540 Ma), which coincides with the opinion of Hengshan complex being the arc root of Wutai arc.

Intensity of reworking-A key factor for formation of large and superlarge gold deposits in greenstone belts and metamorphosed microclastic rocks of China;

With relatively high total gold background values,the strata of the greenstone belt in western Shandong are source beds of gold deposit.

The greenstone belt type gold deposit in the North China craton (NCC), one of the most important deposit types in China, is the major source of gold productions and reserves.