Perea, H.; Masana, E.; Santanach, P. - In: Natural Hazards 39 (2006) 3, pp. 451-477
In intra-plate regions with low-seismic activity, seismic cycles last between 10<Superscript>3</Superscript> and 10<Superscript>5</Superscript> years and, consequently, quiescent faults may be capable of producing catastrophic earthquakes. Paleoseismic studies, which are necessary to define capable faults in these regions and to establish their...</superscript></superscript>