RT Journal Article
T1 Resultados preliminares del estudio paleosísmico mediantetrincheras de la falla de Alhama de Murcia (Cordillera Bética)
A1 Hernández Enrile, José Luis
A1 Martínez Díaz, José Jesús
A1 Masana, Eulàlia
A1 Santanach, Pere
AB Trenching on Alhama de Murcia fault trace has been done in order to identify and quantify paleoseismic deformation on a 100 km long active oblique-slip fault. The first results from one of the trenches confirm the existence of coseism ic reverse fault deformation affecting quaternary alluvial fan deposits. The sedimentary evolution observed on trench shows a temporary blocking of Colmenar creek flow (in the foot wall of the Alhama de Murcia fault), due to uplifting of the hanging wall during coseismic reactivation. An available age of 3010 ± 90 yr post-dated that process.
PB Sociedad Geológica de España.
SN 1576-5172
YR 2000
FD 2000
LK https://hdl.handle.net/20.500.14352/57978
UL https://hdl.handle.net/20.500.14352/57978
LA spa
NO Comisión Interministerial de Ciencia y Tecnología
NO F.A.U.S.T.
DS Docta Complutense
RD 11 abr 2025