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Neotectonic in northern Galicia: Reverse faults with quaternary activity in the fluvial basin of Alfoz (Lugo)

dc.contributor.authorRodríguez García, Augusto
dc.contributor.authorQuintanilla, Luisa
dc.contributor.authorGonzález Menéndez, L.
dc.contributor.authorSuárez Rodríguez, A.
dc.description.abstractIn the weathered depression developed on the A Toxiza variscan granite (northern Galicia) two high angle reverse faults have been located putting the granitic basement over pleistocene fluvial deposits. Several inferred folds are probably related to these NW-SE faults. The location of another reverse fault affecting the granite basement fur ther to the NW allow us to correlate all these faults with a major fault system of NWSE strike known for its recent seismogenic activity in the cantabrian domain. Our results on the analysis of the faults establish an important reverse component in contrast with the normal component calculated for the NW-SE faults of nothern Galicia from seismic data and fault population analysis in previous worksen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.subject.otherReverse faultsen_US
dc.subject.otherFluvial depositsen_US
dc.titleNeotectónica en el norte de Galicia: Fallas inversas de actividad cuaternaria en la cuenca fluvial del alveolo de Alfoz, Lugoen_US
dc.titleNeotectonic in northern Galicia: Reverse faults with quaternary activity in the fluvial basin of Alfoz (Lugo)eng

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