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   geometry of oceanic slab beneath the western makran subduction zone  
   
DOR 20.1001.2.9819010854.1398.8.1.70.7
نویسنده momeni hamid reza ,motaghi khalil ,rahmani mohsen ,ghods abdolreza ,sobuti farhad
منبع كنفرانس بين المللي زلزله شناسي و مهندسي زلزله - 1398 - دوره : 8 - هشتمین کنفرانس زلزله شناسی و مهندسی زلزله - کد همایش: 98190-10854 - صفحه:1 -2
چکیده    We present a seismic velocity image for the makran upper mantle (se iran) across a profile (aa', in figure 1) extending from chabahar to the north of taftan volcanic mountain. the image was generated by a teleseismic travel time tomography called the ach method (aki et al., 1977).
کلیدواژه makran ,tomography ,ach method ,subduction slab geometry
آدرس institute for advanced studies in basic sciences, iran, institute for advanced studies in basic sciences, iran, institute for advanced studies in basic sciences, iran, institute for advanced studies in basic sciences, iran, institute for advanced studies in basic sciences, iran
پست الکترونیکی farhads@iasbs.ac.ir
 
     
   
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