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The Formation Age of the Granite-porphyry and Its Geological Significance in Shiyazi of Fang County

SHI Xianbin;DENG Qianzhong;Hubei Geological Survey;  
In contiguous area of the south Qinling orogenic belt and Yangtze craton,the authors did the regional geological survey on the scale 1∶ 50 000 and then,the granitoid intrusion was discovered in Shiyazi of Fang County. By the way of the characters of the field geology of rock body,and the geochemical characters of the rock,and geochemical isotopic study with geochronological characters,the magmatic origin and tectonic environment of the rocks formation was discussed. By means of the zircon U-Pb isotopic method,the weighted mean206 Pb /238 U age is reported in this paper,which is722. 9 ± 6 Ma,it was indicated the rocks formed in the Jinningian movement. According to the geochemical characters of the rock,the granite porphyry might be formed in rift valley,which deepen the research tectonic-thermal event in the South Qinling orogenic belt.
【Fund】: 中国地质调查局国土资源大调查项目(1212011120782)
【CateGory Index】: P588.12
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