000012266 001__ 12266
000012266 005__ 20141205160036.0
000012266 04107 $$aeng
000012266 046__ $$k2008-10-12
000012266 100__ $$aZaré, Mehdi
000012266 24500 $$aBalakot, Muzaffarabad Earthquake of 8 October 2005, Mw 7.6; Field Observations on Geological Aspects

000012266 24630 $$n14.$$pProceedings of the 14th World Conference on Earthquake Engineering
000012266 260__ $$b
000012266 506__ $$arestricted
000012266 520__ $$2eng$$aThis article is focused on the geological observations in the meizoseismal region in Muzaffarabad earthquake, Oct..8 2005, Mw 7.6. The major damaged area (the valley elongated between Balakut, Muzaffarabad and and Bagh) was elongated parallel to the reactivated Muzaffarabad fault and the attenuation is high in the direction normal to the fault comparing with the direction parallel to it. The high intensity values were assessed in the localities where some huge landslides are observed.

000012266 540__ $$aText je chráněný podle autorského zákona č. 121/2000 Sb.
000012266 653__ $$aMuzaffarabad, Pakistan, Reconnaissance, Geology, Intensity, Attenuation

000012266 7112_ $$a14th World Conference on Earthquake Engineering$$cBejing (CN)$$d2008-10-12 / 2008-10-17$$gWCEE15
000012266 720__ $$aZaré, Mehdi$$iKarimi-Paridari, Sepideh
000012266 8560_ $$ffischerc@itam.cas.cz
000012266 8564_ $$s1034104$$uhttps://invenio.itam.cas.cz/record/12266/files/01-1044.pdf$$yOriginal version of the author's contribution as presented on CD, Paper ID: 01-1044.
000012266 962__ $$r9324
000012266 980__ $$aPAPER