RT Journal Article
T1 Actividad tectónica cuaternaria en la Cuenca de Huércal-Overa (Almería, Sureste de España): deformaciones asociadas a la falla de Albox
A1 García Meléndez, Eduardo
A1 Goy Goy, José Luis
A1 Zazo Cardeña, Caridad
AB The main Quaternary tectonic ativity in the Huércal-Overa Basin is related to the Albox fault, which extends from Tljola in the Almanzora Corridor (SSW) to the eastern Huércal-Overa Basin (NNE), In this work an example of the effects of the fault movement both in the sediments and in the relief is presented linked to a fault segment in the Alto de Ruchete area, Analysis of deformation structures related to the main fault present in the Quaternary sediments, such as smalf and medium reverse faults, monoclinal folds, drag-folds and scarps, alfow the establishment of an evolution model during the Quaternary for the tectonic and sedimentary activity and their effects in the relief genesis.
PB Sociedad Geológica de España
SN 0213-683X
YR 2004
FD 2004
LK https://hdl.handle.net/20.500.14352/120418
UL https://hdl.handle.net/20.500.14352/120418
LA spa
NO García Meléndez, Eduardo, et al. «Actividad tectónica cuaternaria en la Cuenca de Huércal-Overa (Almería, Sureste de España): deformaciones asociadas a la falla de Albox». Geogaceta, n.º 36, 2004, pp. 63-66, https://sociedadgeologica.org/publicaciones/geogaceta/geogaceta-36-2004/.
NO Ministerio de Ciencia y Tecnologia (España)
DS Docta Complutense
RD 29 may 2025