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geometry of oceanic slab beneath the western makran subduction zone
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DOR
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20.1001.2.9819010854.1398.8.1.70.7
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نویسنده
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momeni hamid reza ,motaghi khalil ,rahmani mohsen ,ghods abdolreza ,sobuti farhad
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منبع
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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
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چکیده
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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).
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کلیدواژه
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makran ,tomography ,ach method ,subduction slab geometry
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آدرس
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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
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پست الکترونیکی
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farhads@iasbs.ac.ir
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Authors
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