• 责任者：Sun Jinlong (Key Laboratory of Marginal Sea Geology ; South China Sea Institute of Oceanology ; Chinese Academy of Sciences ; Guangzhou 510301 ; China) ; Xu Huilong
• 刊名：Marine Geology & Quaternary Geology
• 出版年：2009
• 卷期：29(3)
• 关键词：新构造运动 ; neotectonic movement ; 动力学 ; dynamics ; 南海 ; South China Sea
• 页码：p.61-68
• 图表：6 illus., 24 refs.
• 分类号：0300
• issnNo：ISSN0256-1492
• isbnNo：CN37-1117/P

According to seismicity, focal mechanism solution (FMS) and GPS data, the authors analyzed the characteristics of the neotectonics in this area, and put forward the dynamic mechanism of the neotectonics. On the basis of these data, it’s suggested that the NW-trending subduction of Philippine Sea Plate had stronger impact on the research area relative to the India-Tibet collision, and led to strong seismicity and NW-trending stress field. However, lateral stress transmission resulting from the collision also affected this area, and caused the South China Block to have moved southeastward.