WordNet
- being where earthquake waves arrive simultaneously (同)coseismal
English Journal
- April 2012 intra-oceanic seismicity off Sumatra boosted by the Banda-Aceh megathrust.
- Delescluse M, Chamot-Rooke N, Cattin R, Fleitout L, Trubienko O, Vigny C.SourceLaboratoire de Géologie, Ecole Normale Supérieure and CNRS UMR8538, 75005 Paris, France. delescluse@geologie.ens.fr
- Nature.Nature.2012 Oct 11;490(7419):240-4. doi: 10.1038/nature11520. Epub 2012 Sep 26.
- Large earthquakes nucleate at tectonic plate boundaries, and their occurrence within a plate's interior remains rare and poorly documented, especially offshore. The two large earthquakes that struck the northeastern Indian Ocean on 11 April 2012 are an exception: they are the largest strike-slip eve
- PMID 23023134
- Under the hood of the earthquake machine: toward predictive modeling of the seismic cycle.
- Barbot S, Lapusta N, Avouac JP.SourceDivision of Geological and Planetary Sciences, California Institute of Technology, 1200 East California Boulevard, Pasadena, CA 91125, USA. sbarbot@caltech.edu
- Science (New York, N.Y.).Science.2012 May 11;336(6082):707-10.
- Advances in observational, laboratory, and modeling techniques open the way to the development of physical models of the seismic cycle with potentially predictive power. To explore that possibility, we developed an integrative and fully dynamic model of the Parkfield segment of the San Andreas Fault
- PMID 22582259
Japanese Journal
- 1707年宝永地震による浜名湖北部の沈降と大坂の被害数 (特集 第21回GSJシンポジウム 古地震・古津波から想定する南海トラフの巨大地震)
- 矢田 俊文
- GSJ地質ニュース = GSJ chishitsu news 2(7), 208-211, 2013-07
- NAID 40019752312
- Coseismic dehydration of serpentinite: Evidence from high-velocity friction experiments
- Lin Aiming,Takano Soichiro,Hirono Tetsuro,Kanagawa Kyuichi
- Chemical Geology 344, 50-62, 2013-04-19
- … These findings show that dehydration reactions of serpentine can be caused by frictional heating that accompanies frictional melting in the slip zone, and by the rapid diffusion of frictional heat from the main slip zone to a wide zone bounded by the coseismic slip plane during seismic faulting. …
- NAID 120005347087
- InSARで捉えた2010年イラン南東部の地震に伴う地殻変動と断層モデルの推定
- KOBAYASHI Tomokazu,TOBITA Mikio,SUZUKI Akira [他]
- Bulletin of the Geospatial Information Authority of Japan 60, 7-17, 2013-03
- NAID 40019615149
Related Links
- co·seis·mal (k -s z m l, -s s -) also co·seis·mic (-m k). adj. Relating to or designating a line connecting the points on a map that indicate the places simultaneously affected by an earthquake shock. n. A coseismal line.
- adjective. of, pertaining to, or being in a line, curve, etc., connecting or comprising points on the earth's surface at which an earthquake wave arrives simultaneously . Also, co·seis·mic. Origin: 1850–55; co- + seismal. Dictionary.com Unabridged ...
Related Pictures
