ISSN 1006-3021 CN11-3474/P
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红河断裂的GPS监测
  
关键词:The Red River fault  GPS  horizontal movement
基金项目:中国地质调查局项目“青藏高原东部现代地壳运动GPS监测”(编号:200416000003)
作者单位
张清志 成都地质矿产研究所四川成都610082 
刘宇平 成都地质矿产研究所四川成都610082 
陈智粱 成都地质矿产研究所四川成都610082 
唐文清 成都地质矿产研究所四川成都610082 
张选阳 成都地质矿产研究所四川成都610082 
Robert W.KING 麻省理工学院坎布里奇麻萨诸塞美国02139 
Barrcel C.BURCHFIEL 麻省理工学院坎布里奇麻萨诸塞美国02139 
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摘要:
GPS Monitoring along the Red River Fault
      The Red River fault zone is a gigantic sliding fault zone. On the basis of GPS observations in Yunnan in 1999 and 2003, the velocity vector diagram was drawn against the Eurasia reference framework. The average velocity is 3.726 mm/a in east direction and-9.013 mm/a in north direction. The velocity component of the GPS stations in the north is reduced from north to south, and that in the east is reduced from west to east. In the surveying zone, the GPS stations show obvious extensional and right_lateral strike_slip movement. An analysis of the features of the horizontal movement in the Red River zone reveals that the faulting activity characteristics are quite consistent with geological results.
ZHANG Qing-zhi,LIU Yu-ping,CHEN Zhi-liang,TANG Wen-qing,ZHANG Xuan-yang,Robert W.KING,Barrcel C.BURCHFIEL.2006.GPS Monitoring along the Red River Fault[J].Acta Geoscientica Sinica,27(4):367-372.
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