Titlebook: Earthquake Hazard and Risk; Vladimír Schenk Book 1996 Kluwer Academic Publishers 1996 Geoinformationssysteme.aftershock.earthquake.microse

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Importance of Geological Data in Probalistic Seismic Hazard Assessments: A Case Study from ETNE, Wesments through an example from Etne in western Norway..Detailed lineament studies conducted on satellite images, have revealed possible active fault zones in the Sunnhordland District, including the Etne Fault Zone (EFZ). The parallelism between a recently discovered NW-SE trending regional aeromagne

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1878-9897 nterested in earthquake hazard andseismic risk research as well as a more general audience ofseismologists, geophysicists and Earth scientists. It is also usefu978-94-010-6592-4978-94-009-0243-5Series ISSN 1878-9897 Series E-ISSN 2213-6959

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https://doi.org/10.1057/9780230618558nergy was released at the beginning of the sequence, with the highest magnitude M. = 3.6. Most events were felt by the population, but they caused no damage..Fault plane solutions calculated for a selected number of events show that most of the mechanisms have T axes oriented in an anti-apenninic di

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David Nightingale,Christopher Spencern at two stages of post-seismic activity: an intensive fissuring, leading to formation of blocks on a different scale (from metres to kilometres), and a consolidation of aftershock zone by smoothing of tectonic stress gradients at the block boundaries.

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Susanne MacGregor,Betsy Ettorre, classification of dependent and independent events, normalization of the earthquake regime per period of observation and/or the size of the area under study, and application of different attenuation laws, effects of near-surface sedimentary deposits) upon the final hazard values have been taken in

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