joint analysis of the alos-2 and sentinel-1a data on the 2017 sefid sang earthquake, northeastern iran
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DOR
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20.1001.2.9819010854.1398.8.1.108.5
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نویسنده
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ghayournajarkar nematollah ,fukushima yo
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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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The iranian plateau is deformed between the converging arabian and eurasian plates. their convergence is principally taken up by the active makran subduction zone to the south, in addition to shortening and strike-slip faulting accommodated by crustal structures, which are non-uniformly distributed in several continental deformation domains such as the zagros, alborz and kopeh dagh mountain ranges.
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کلیدواژه
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sefid sang earthquake ,insar ,alos-2 ,sentinel-1a ,coseismic deformation
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آدرس
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tohoku university, japan, tohoku university, japan
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پست الکترونیکی
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fukushima@irides.tohoku.ac.jp
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