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《Journal of Jiling University (Earth Science Edition)》 1992-02
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RELATIONSHIP AMONG THE FOUR GROUPS AT THREE MOUNTAINS

Xu Chaolei Xu Youhua(Regional Geologic Survey Party, Shanxi Bureau of Geology and Mineral Resources)  
Four series of precambrian metamorphic rocks have been recognized in Wutai Mt. and the adjacent Taihang Mt. Hengshan. The low metamorphosed Hutuo Gr. with its thick bottom conglomerate overlies unconformably on wutai Gr. Hengshan complexes belong to deeply metamorphosed part of Wutai Gr. Low-middle metamorphosed Wutai Gr. which drived from volcanic rocks is thrown up on Fuping Gr. toward east. The Fuping Gr. undergo metamorphism of high amphibolite facies is formed by Carbonate formation. Both the Wutai Gr. and the Fuping Gr. are synchronous out-of-phase deposits. In the past, the nappe ductile shear zone between them was regarded clastic rock of the bottom of Wutai Gr..Largely distributed gray gneiss in Hengshan complex and Fuping Gr. intruded during Wutai period. The Wutai Gr. Fuping Gr. and Hengshan Complex construct the crystalltine basement at 2800Ma. They were folded. metamorphosed and finally intruded by the gray gneiss at 2500Ma.
【CateGory Index】: P588. 3
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