2026-06-27T15:35:36Zhttps://docta.ucm.es/rest/oai/request

oai:docta.ucm.es:20.500.14352/580922023-07-14T00:41:06Zcom_20.500.14352_14col_20.500.14352_15

Rodríguez Pascual, Manuel Barrera, José Luis 2023-06-20T17:19:04Z 2023-06-20T17:19:04Z 2002 0213-683X https://hdl.handle.net/20.500.14352/58092 Paleoseismic structures are described far the first time in the volcanism of Campo de Calatrava. The structures are located in hydromagmatic deposits of maars. This study allows to detect seismic activity after the last Quaternary eruptions in the Granatura - Moral Basin (Neogene Age). The liquefied sediments are conglomerates (lapilli) and the seismic magnitude to fiquely this coarse-grained sediment should be higher than 7.5. spa open access Estructuras paleosísmicas en depósitos hidromagmáticos del vulcanismo neógeno del Campo de Calatrava, Ciudad Real (España) journal article