Seismic hazard assessment of the Kivu rift segment based on a new sismo-tectonic zonation model (Western Branch of the East African Rift system)
| dc.contributor.author | Havenith, H.-B. | |
| dc.contributor.author | Delvaux, D. | |
| dc.coverage.spatial | Africa - Central | |
| dc.date | 2015 | |
| dc.date.accessioned | 2016-03-15T10:07:53Z | |
| dc.date.available | 2016-03-15T10:07:53Z | |
| dc.identifier.uri | https://orfeo.belnet.be/handle/internal/2581 | |
| dc.description | In the frame of the Belgian GeoRisCA multi-risk assessment project focused on the Kivu and Northern Tanganyika Region, a seismic hazard map has been produced for this area. It is based on a on a recently re-compiled catalogue using various local and global earthquake catalogues. The use of macroseismic epicenters determined from felt earthquakes allowed to extend the time-range back to the beginning of the 20th century, thus spanning about 100 years. The magnitudes have been homogenized to Mw and the most obvious aftershocks removed. We defined a relatively fine seismo-tectonic zonation in 10 seismic source zones considering the geological structure, neotectonic fault systems, basin architecture and distribution of seism epicenter. On the basis of the filtered seismic catalogue including only main shocks, Gutenberg-Richter Laws have been defined for the entire area and for each sub-zone. On the basis of this seismo-tectonic information and existing attenuation laws that had been established by Twesigomwe (1997) and Mavonga et al. (2007) for this area, seismic hazard has been computed with the Crisis 2012 (Ordaz et al., 2012) software. The outputs of this assessment clearly show higher PGA values (for 475 years return period) along the Rift than the previous estimates by Twesigomwe (1997) and Mavonga (2007) while the same attenuation laws had been used. The main reason for these higher PGA values is likely to be related to the more detailed zonation of the Rift structure marked by a strong gradient of the seismicity from outside the rift zone to the inside. Mavonga, T. (2007). An estimate of the attenuation relationship for the strong ground motion in the Kivu Province, Western Rift Valley of Africa. Physics of the Earth and Planetary Interiors 62, 13 21. Ordaz M, Martinelli F, Aguilar A, Arboleda J, Meletti C, D Amico V. (2012). CRISIS 2012, Program for computing seismic hazard. Instituto de Ingeniería, Universidad Nacional Autónoma de México. Twesigomwe, E. (1997). Probabilistic seismic hazard assessment of Uganda, Ph.D. Thesis, Dept. of Physics, Makare University, Uganda. | |
| dc.language | eng | |
| dc.title | Seismic hazard assessment of the Kivu rift segment based on a new sismo-tectonic zonation model (Western Branch of the East African Rift system) | |
| dc.type | Conference | |
| dc.subject.frascati | Earth and related Environmental sciences | |
| dc.audience | Scientific | |
| dc.subject.free | Geodynamics and mineral resources | |
| dc.source.title | EGU General Assembly 2015, Vienna | |
| dc.source.volume | Geophysical Research Abstracts, 17 | |
| dc.source.page | EGU2015-6082 | |
| Orfeo.peerreviewed | No | |
| dc.identifier.rmca | 4300 |
