The seismic deformation zone of M 7.6 Lancang earthquake in 1988 is mainly composed of a series of surface ruptures and distributed along the Muga and Datangzi faults, The mechanical property of right-lateral shear of the deformation zone is analysed.

 
  • 澜沧7.;6级地震形变带主要以地震裂缝带的形式出现;未发现有类似耿马7
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