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《Geotectonica Et Metallogenia》 2009-03
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Application of Acoustic Emission in the Study of Paleo-Tectonic Events in the Northern Part of Tanlu Fracture

XIE Guoai,WANG Xiyong,ZHANG Qinglong,WANG Liangshu and XU Shiyin(School of Earth Sciences and Engineering,Nanjing University,Nanjing 210093,Jiangsu,China)  
By using acoustic emission to study the paleo-tectonic events field in the north segment of the Tanlu fracture,the result indicates that this area has undergone eight paleo-tectonic movements since Late Ordovician. The maximum principal stress value has been determined as 153.6 MPa. There were no or weak tectonic movements from Early Permian to the early Yanshan movement. There were four paleo-tectonic movements after Early Cretaceous. AE results show that the Yilan-Yitong and Haerbing-Changchun faults were formed in the Proterozic,then the movment stopped. The Tanlu fracture strongly moved in the Yanshan period,and became a large-scale strike-slip fault.
【Fund】: 中国石化项目“松辽盆地南部断陷层构造沉积特征研究”(DBKT2006-YJ-022)资助
【CateGory Index】: P542.3
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