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《JOURNAL OF CHANGCHUN UNIVERSITY OF SCIENCE AND TECHNOLOGY》 1999-04
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PROGRESSIVE COALESCENCE MODEL OF BRITTLE FAULT FORMATION

Tang Shijia,Peng Ensheng,Sun Zhenjia (Insititute of Geology, Central South University of Technology, Changsha 410083)  
In lower crust, faults often consist of a series of secondary fractures. Based on experimental microfeatures in rock mechanics and macrostructures in fields, authors set up the progressive coalescence model which is from microcrack,stylolitic fracture, large fault to superlarge fault in fault formation, analyse the forming mechanism of progressive coalescence model, and explain three phenomenon, respectively, the undulation,branch of fault and that the angle between fractures and principal axis decreases gradually.
【Fund】: 国家教委博士点基金
【CateGory Index】: P542.3
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