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《Chinese Journal of Geology(Scientia Geologica Sinica)》 2006-02
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~(40)Ar-~(39)Ar GEOCHRONOLOGY RECORDS OF TRANSITION FROM STRIKE-SLIP TO EXTENSION IN THE TAN-LU FAULT ZONE ON EASTERN TERMINAL OF THE DABIE MOUNTAINS

Wang Yongsheng Zhu Guang Song Chuanzhong Liu Guosheng Xiang Biwei Li Changcheng Xie Chenglong(College of Resources and Environmental Engineering, Hefei University of Technology, Hefei 230009)  
So far there is a dispute on active modes and time of the Tan-Lu fault zone. This paper used ~ 40 Ar-~ 39 Ar geochronology to study the samples of muscovite, biotite, plagioclase or K-feldspar from the mylonites along the sinistral Tan-Lu ductile shear zone on eastern terminal of the Dabie Mountains. It was discovered that the Tan-Lu fault zone acted as a sinistral strike-slip one before 139 Ma, then became an extensional one. Our work revealed that the transition time might be 128~139 Ma ago. In the course of extension, the Tan-Lu ductile shear zone experienced slowly rift and cooling, which caused the minerals with less closure temperature recorded small ages. The ~ 40 Ar-~ 39 Ar ages of 110 Ma of the biotite and 97~92 Ma of the plagioclase indicated that the extension activity of the Tan-Lu fault zone continued to about 90 Ma.
【Fund】: 国家自然科学基金资助项目(批准号:40272094)。
【CateGory Index】: P597.3
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