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Dong Yingjun Xue Guangqi Ma Kaiyi Jiang Mei (Chinese Academy of Geological Sciences,Beijing 100037)  
Lithosperic anisotropy has been studied using the data of SKS wave recorded at the 3-component stations that were deployed by the Sion-French cooperative seismic experiment in northeastern Tibetan Plateau. Results indicate fairly big differences between anisotropical features of north and south sides of Altyn Fault System. Fast directions near Altyn Fault System average N80°E,whereas it is about N45°W beneath the Qaidam basin. In addition,the former is stronger than the latter,which is a striking indication of oriented material movement deep beneath the Altyn Fault System.
【Fund】: 中法合作项目
【CateGory Index】: P542.3
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