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Earthquake recurrence intervals from lacustrime varved dediments of upper miocene age. Hijar basin (Albacete)

dc.contributor.authorRodríguez Pascua, M. A.
dc.contributor.authorVicente, Gerardo de
dc.contributor.authorRamírez Rayo, M. S.
dc.contributor.authorMartín Velázquez, Silvia
dc.contributor.authorCalvo, J. Pedro
dc.description.abstractPaleoseismic imprimt in lacustrine varved sediments (Upper Miocene) has been made in the Hijar Basin (External Prebetic, Albacete). Mixed layers related to seismic activity have been observed in the varved sediments. These deformational structures are associated with earthquake's magnitude 3 5.5. Each varve may be considered as annual laminae and used to date the time among deformation structures. The average recurrence interval for these study section is 119 years (± 33 years of standard desviation) for 1189 recorded years.en_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.subject.otherMixed layersen_US
dc.subject.otherLacustrine varved sedimentsen_US
dc.subject.otherHijar basinen_US
dc.titlePeríodos de recurrencia de paleoterremotos en sedimentos varvados lacustres del Mioceno superior. Cuenca de Híjar (Albacete)en_US
dc.titleEarthquake recurrence intervals from lacustrime varved dediments of upper miocene age. Hijar basin (Albacete)eng

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