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《JOURNAL OF CHENGDU UNIVERSITY OF TECHNOLOGY》 1998-04
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THE CHARACTERISTICS AND GENESIS OF THE BASIC INTRUSIVE COMPLEX IN CHENGJIANG PERIOD, MICANGSHAN, SICHUAN

Xiao Yuanfu, Ma Runze, Wei Xiangui, He Zhengwei, Li Youguo (Chengdu University of Technology, China)  
According to the ivestigation and study of the magmatic complex in Micangshan area, and using the theory of the same source magma evolution, the Chengjiang period intrusive complex has been confirmed for the first time. The Yunwushan super unit is the reslut of magmatism early during the period and consists of four units. Isotopic age is 776.5 Ma to 766.7 Ma, and the petrochemical characteristics are rich in TiO 2, Al 2O 3 and (FeO), SI=40~15, DI=11~56, σ =1.8~3.7. REE and trace elements show that each unit is the result of the same source magma evolution. The temperature of original magma is between 850℃ and 1125℃. The diagenetic pressure is about 0.710 ~0.756 GPa, f O 2 ≥10 -11 , and the magma came from the mantle melting and mixed mantle and lower crust. The basic intrusive complex is the result of the mantle diapiric uprise in the middle stage of the rift faulting during the early Sinian Period.
【CateGory Index】: P588.124
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