2026-03-07T00:32:57Z https://repository.dl.itc.u-tokyo.ac.jp/oai

oai:repository.dl.itc.u-tokyo.ac.jp:00032537 2022-12-19T05:38:00Z 80:4535:4613:4614 9:504:4538:4615:4616

イラン南部のバム断層において2003年12月26日バム地震によって生じた地表変位 Surface effects of the December 26th,2003 Bam earthquake along the Bam fault in southeastern Iran Okumura, Koji 125452 Kondo, Hisao 125453 Azuma, Takeshi 125454 Echigo, Tomoo 125455 Khaled, Hessami 125456 51.1 surface rupture Quaternary fault fault scarp Bam earthquake southeastern Iran application/pdf During the December 26th, 2006 Bam earthquake, continuous ruptures with a consistent rightlateral strike-slip of a few centimeters occurred north of Bam. A 3km long strand of ruptures coincides exactly with the trace of the geologic Bam fault. These ruptures were possibly caused by the tectonic slip on the source fault of the 2006 earthquake. The Bam scarp south of the Zehedan highway might have grown during the earthquake. The extension of the area around the scarp indicated by the scarp-parallel fissures may represent the coseismic stretch of the surface. South of the Bam scarp, there was no systematic surface effect. The absence of significant tectonic offset at the surface is concordant with the intermediate magnitude of Mw 6.6 Only a small and deep portion of the Bam fault, or another adjacent blind fault plane was ruptured in 2006. The geologic evidence of the over 50km long Bam fault suggests a large, probably M 7.5 or larger, event in the future, however, there is no historic and geologic data to quantify the risks. departmental bulletin paper 東京大学地震研究所 2004 application/pdf 東京大學地震研究所彙報 = Bulletin of the Earthquake Research Institute, University of Tokyo 3-4 79 29 36 AN00162258 00408972 https://repository.dl.itc.u-tokyo.ac.jp/record/32537/files/IHO79301.pdf https://doi.org/10.15083/0000032537 http://hdl.handle.net/2261/5756 https://repository.dl.itc.u-tokyo.ac.jp/records/32537 eng