Zobrazeno 1 - 10
of 12
pro vyhledávání: '"V. Swaroopa Rani"'
Publikováno v:
Nonlinear Processes in Geophysics, Vol 17, Iss 5, Pp 569-574 (2010)
The complexity in the tsunami phenomenon makes the available warning systems not much effective in the practical situations. The problem arises due to the time lapsed in the data transfer, processing and modeling. The modeling and simulation needs th
Externí odkaz:
https://doaj.org/article/0290e5b6da1c4d07b15ab44471180bfe
Publikováno v:
Natural Hazards. 77:97-107
The Andaman–Sumatra is one of the seismically active subduction zones and experienced three largest earthquakes in the recent past and rupturing more than 1,600-km-long portion of the plate boundary. The seismicity analysis of these large earthquak
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9e0759cdecb456f9c254c07d6f59ceed
https://doi.org/10.1007/s11069-014-1143-2
https://doi.org/10.1007/s11069-014-1143-2
Publikováno v:
Natural Hazards. 63:211-221
The Andaman-Sumatra arc is an active subduction zone and had generated several destructive tsunamis in the past. The 2004 Indian Ocean tsunami has led to more and more paleotsunamic research of identifying geological evidences of past submergence. Th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3f056eccc7f786ca90172a8b0415ca4e
https://doi.org/10.1007/s11069-011-9946-x
https://doi.org/10.1007/s11069-011-9946-x
Publikováno v:
Marine Geodesy. 34:77-82
During the last three decades, the eastern segment of the Makran subduction zone has been more active than the western segment. We analyze Makran seismicity using the NEIC catalog from 1973 to 2008. A temporal decrease of b-value in eastern Makran in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d8427df9f6b8a1be07365f075171e606
https://doi.org/10.1080/01490419.2011.547804
https://doi.org/10.1080/01490419.2011.547804
Publikováno v:
Marine Geodesy. 34:48-58
The Sumatra-Andaman arc is an active subduction zone that has generated several destructive tsunamis. The December 26, 2004, Sumatra-Andaman earthquake of magnitude Mw∼9.3 generated the most destructive tsunami known to man. The sustained high wate
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::415a53bf9ec502f8de635b215a55c339
https://doi.org/10.1080/01490419.2011.547802
https://doi.org/10.1080/01490419.2011.547802
Publikováno v:
Nonlinear Processes in Geophysics, Vol 17, Iss 5, Pp 569-574 (2010)
The complexity in the tsunami phenomenon makes the available warning systems not much effective in the practical situations. The problem arises due to the time lapsed in the data transfer, processing and modeling. The modeling and simulation needs th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ee2fc023aab22fb7c00db6e2b7069532
https://doi.org/10.5194/npg-17-569-2010
https://doi.org/10.5194/npg-17-569-2010
Publikováno v:
Computers & Geosciences. 35:2095-2099
Determination of the thermo-mechanical structure of the crust for seismically active regions using available geophysical and geological data is of great importance. The most important feature of the intraplate earthquakes in the Indian region are tha
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b7c327cf3949750117c5013aea7a4710
https://doi.org/10.1016/j.cageo.2008.12.013
https://doi.org/10.1016/j.cageo.2008.12.013
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