摘要
The intermediate volcanic rocks of Dahalajunshan Group in southeast Tekesi County area, west Tianshan Mountains, are calc-alkaline volcanic rocks, most of them are basaltic andesite, andesite, with minor trachyandesite. These rocks are high in silicon and sodium, low in titanium and potassium. Geochemical characteristics show that the magmatic source is of enriched mantle magma source,which was resulted from by crust contamination and metasomatic process by fluid or melted materials from subduction residual plate.