000011102 001__ 11102
000011102 005__ 20141205155836.0
000011102 04107 $$aeng
000011102 046__ $$k2008-10-12
000011102 100__ $$aNagumo, Hideki
000011102 24500 $$aSource Process of the 2006 Oita-Chubu Earthquake (Mw6.4) Occurring in the Philippine Sea Slab

000011102 24630 $$n14.$$pProceedings of the 14th World Conference on Earthquake Engineering
000011102 260__ $$b
000011102 506__ $$arestricted
000011102 520__ $$2eng$$aWe investigate source characteristics of a moderate-size intermediate-depth earthquake (MW6.4) occurring on 12 June, 2006 at a depth of about 145km in the Philippine Sea slab subducting beneath the Kyushu district, Japan. First we investigate rupture process from waveform inversion of strong ground motion and teleseismic body wave data. The result shows complex source process of this earthquake. We extract two asperities form the inversion result. Next we estimate the short period level of S-wave acceleration source spectrum. Estimated short period level is consistent with typical level estimated from other intraslab events, which is higher than that of crustal and interplate earthquake. 2006 Oita-chubu earthquake, intraslab earthquake, waveform inversion, spatio-temporal slip distribution, asperity model

000011102 540__ $$aText je chráněný podle autorského zákona č. 121/2000 Sb.
000011102 653__ $$a

000011102 7112_ $$a14th World Conference on Earthquake Engineering$$cBejing (CN)$$d2008-10-12 / 2008-10-17$$gWCEE15
000011102 720__ $$aNagumo, Hideki$$iSasatani, Tsutomu
000011102 8560_ $$ffischerc@itam.cas.cz
000011102 8564_ $$s1719347$$uhttps://invenio.itam.cas.cz/record/11102/files/02-0145.pdf$$yOriginal version of the author's contribution as presented on CD, Paper ID: 02-0145.
000011102 962__ $$r9324
000011102 980__ $$aPAPER