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华北克拉通南缘登封地区嵩山石英岩中3.40 Ga碎屑锆石的发现及其地质意义

BULLETIN OF MINERALOGY, PETROLOGY AND GEOCHEMISTRY(2008)

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Abstract
1950年,张伯声在登封市东北发现太古宙登封群与元古宙嵩山群,元古宙五指岭片岩与震旦系之间分别呈角度不整合,并将这两个不整合命名为"嵩阳运动(五台运动)"和"中条运动"(张伯声,1951;孙勇等,1986).
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