Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/1337
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dc.contributor.authorallMidzi, V.; Goetz Observatory, Department of Meteorology, Ascot, Bulawayo, Zimbabween
dc.contributor.authorallHlatywayo, D. J.; Applied Physics Department, Faculty of Applied Sciences, Bulawayo, Zimbabween
dc.contributor.authorallChapola, L. S.; Geological Survey of Malawi, Zomba, Malawien
dc.contributor.authorallKebede, F.; Geophysical Observatory, Faculty of Sciences, Addis Ababa University, Addis Ababa, Ethiopiaen
dc.contributor.authorallAtakan, K.; Kuvvet Atakan Institute of Solid Earth Physics, University of Bergen, Norwayen
dc.contributor.authorallLombe, D. K.; Geological Survey of Zambia, Geological Section, Lusaka, Zambiaen
dc.contributor.authorallTuryomurugyendo, G.; Department of Geological Survey and Mines, Entebbe, Ugandaen
dc.contributor.authorallTugume, F. A.; Department of Geological Survey and Mines, Entebbe, Ugandaen
dc.date.accessioned2006-07-26T12:32:41Zen
dc.date.available2006-07-26T12:32:41Zen
dc.date.issued1999-12en
dc.identifier.urihttp://hdl.handle.net/2122/1337en
dc.description.abstractSeismic hazard assessment for the Eastern and Southern Africa region was done using the probabilistic approach. Seismic hazard maps for 10% exceedance in 50 years, 10% exceedance in 100 years, as well as for 50 and 100 years return periods were prepared using the FRISK88M software. The area involved covers a wide region bounded by latitudes 40°S-25°N and longitudes 10°E and 55°E. Input parameters for the computations were obtained using the recent earthquake catalogue compiled by Turyomurugyendo. The catalogue which covers the time period 627-1994, contains earthquakes within the area bounded by 40°S-25°N and 10°E-55°E, with homogeneous magnitudes (M S ). Since a Poisson model of earthquake occurrence is assumed, dependent events were cleaned from the catalogue. Attenuation relations for the Eastern and Southern Africa region based on the strong motion data are virtually non-existent. However, attempts have been made recently by Jonathan and Twesigomwe to establish an average attenuation relation for the region. These relations were used in the computations. Possible uncertainties in the attenuation relations were accounted for using the logic-tree formalism. The results are presented in seismic hazard maps in terms of Peak Ground Acceleration (PGA) for the mean and the 85th percentile. The distribution of PGA values indicate relatively high hazard along the East African rift system. In the northern segments of the rift system, they exceed 250 gals for 10% probability of exceedence in 50 years.en
dc.format.extent5106674 bytesen
dc.format.mimetypeapplication/pdfen
dc.language.isoEnglishen
dc.relation.ispartofseries6/42 (1999)en
dc.subjectSeismic hazard assessmenten
dc.subjectAfrican riften
dc.subjectearthquakeen
dc.subjectUN/IDNDRen
dc.titleSeismic hazard assessment in Eastern and Southern Africaen
dc.typearticleen
dc.type.QualityControlPeer-revieweden
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.99. General or miscellaneousen
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.11. Seismic risken
dc.description.journalTypeJCR Journalen
dc.description.fulltextopenen
dc.contributor.authorMidzi, V.en
dc.contributor.authorHlatywayo, D. J.en
dc.contributor.authorChapola, L. S.en
dc.contributor.authorKebede, F.en
dc.contributor.authorAtakan, K.en
dc.contributor.authorLombe, D. K.en
dc.contributor.authorTuryomurugyendo, G.en
dc.contributor.authorTugume, F. A.en
dc.contributor.departmentGoetz Observatory, Department of Meteorology, Ascot, Bulawayo, Zimbabween
dc.contributor.departmentApplied Physics Department, Faculty of Applied Sciences, Bulawayo, Zimbabween
dc.contributor.departmentGeological Survey of Malawi, Zomba, Malawien
dc.contributor.departmentGeophysical Observatory, Faculty of Sciences, Addis Ababa University, Addis Ababa, Ethiopiaen
dc.contributor.departmentKuvvet Atakan Institute of Solid Earth Physics, University of Bergen, Norwayen
dc.contributor.departmentGeological Survey of Zambia, Geological Section, Lusaka, Zambiaen
dc.contributor.departmentDepartment of Geological Survey and Mines, Entebbe, Ugandaen
dc.contributor.departmentDepartment of Geological Survey and Mines, Entebbe, Ugandaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptGoetz Observatory, Department of Meteorology, Ascot, Bulawayo, Zimbabwe-
crisitem.author.deptApplied Physics Department, Faculty of Applied Sciences, Bulawayo, Zimbabwe-
crisitem.author.deptGeological Survey of Malawi, Zomba, Malawi-
crisitem.author.deptGeophysical Observatory, Faculty of Sciences, Addis Ababa University, Addis Ababa, Ethiopia-
crisitem.author.deptUniversity of Bergen, Norway-
crisitem.author.deptGeological Survey of Zambia, Geological Section, Lusaka, Zambia-
crisitem.author.deptDepartment of Geological Survey and Mines, Entebbe, Uganda-
crisitem.author.deptDepartment of Geological Survey and Mines, Entebbe, Uganda-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
Appears in Collections:Annals of Geophysics
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