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Sm-Nd AGE OF THE UPPERMOST STRATA OF THE WUTAI GROUP, LULIANG Mt. AREA AND THE SPECIFIC PHEATURE OF MANTLE AT THE MAGMATIC SOURCE REGION

Zhang Qichun;Dong Yibao;Yuan Haihua;Xu Chaolei Chengdu College of Geology Shanxi Regional Geology Team  
Based on the Sm-Nd data obtained in this work, age of the uppermost strata ofthe Wutai Group is recognized as 2471±64 Ma, which indicates that Wutai Groupbelongs to Archaean. High ∈_(Nd)(T) value found in this group and in several otherbasement rocks impleies that a significant mantle heterogeneity has existed sinceArckaean. The depleted history of these rocks are in contradiction with the fact ofrelative enrichment in Nd. The depleted mantle might have been supplemented eitherby degasing fluid which came from lower mantle or by contamination of crustmaterial prduced shortly before the magmatic separation.
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