@article{10272/8511,
year = {2006},
url = {http://hdl.handle.net/10272/8511},
abstract = {A paleoseismological analysis was performed along the La Serrata segment of the Carboneras fault (Eastern
Betics) in order to establish its seismic potential. The site was selected after a general geomorphological
analysis of the whole fault and af ter a near-fault study of the surface geology. Trenches across the fault
exposed colluvial wedges, which evidenced sudden deformation events (paleoear thquakes). The Carboneras
is, thus, a seismogenic fault. Evidence of a minimum of four events in the last 50 ka was detected suggesting
a mean recurrence period of 14 ka. The geometry of the units and S-C structures observed in trenches
indicate a lef t-lateral with some reverse component movement along the fault in its most recent activity},
keywords = {Carboneras Fault},
keywords = {Eastern Betics},
keywords = {Paleoseismology},
keywords = {Trenching},
keywords = {Neotectonics},
title = {Primeras evidencias de paleoterremotos en la falla de Carboneras: estudio paleosismológico en el segmento de La Serrata},
title = {First evidence of paleoearthquakes in Carboneras Fault: A Paleoseismological study in La Serrata},
author = {Moreno, Ximena and Masana, E. and Gràcia, E. and Pallàs, R. and Ruano, Patricia and Coll, Miquel and Stepancíková, P. and Santanach, P.},
}