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1.Single-zircon U-Pb dating of diopside-hornblende-plagioclase leptynite yielded an upper intercept age of 2525 Ma±41 Ma and an lower intercept age of 460 Ma±37 Ma, which represent the age of basic volcanic rocks, i.e. the Buyant Group-complex, and the age of emplacement of the Ordovician magma and modification of the Buyant Group-complex, respectively.
同位素年代测试显示,透辉角闪斜长变粒岩单颗粒锆石U-Pb测年获得的不一致线上交点年龄为(2525±41)Ma代表了基性火山岩即宝音图岩群的形成时代不一致线下交点年龄(460±37)Ma代表了奥陶纪岩浆侵位及宝音图岩群的变质改造年龄。收藏指正
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