Persona: Lario Gómez, Javier
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0000-0002-2582-5354
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Lario Gómez
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Javier
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Publicación Registro geológico de tsunamis en el SW Peninsular durante el Holoceno(2010) Zazo Cardeña, Caridad; Goy Goy, José Luis; Silva, Pablo Gabriel; Bardají Azcárate, Teresa; Cabero, Ana; Dabrio, Cristino José; Lario Gómez, JavierDesde la década de los 90 se ha incrementado el estudio de eventos marinos de alta energía que alcanzaron la costa del Golfo de Cádiz, principalmente con el estudio sedimentológico, paleontológico y geomorfológico de sus depósitos (en estuarios, marismas y flechas litorales). El estudio sedimentario y geomorfológico ha permitido identificar Eventos de Oleaje Extremo (Extreme Wave Events, EWE´s) asociados tanto a grandes tormentas como a tsunamis. Investigaciones recientes llevadas acabo en la plataforma del SW Peninsular han utilizado el registro de turbiditas como indicador de actividad paleosísmica. El registro de los eventos costeros y los de plataforma indican que al menos cinco tsunamis generados por grandes terremotos (Mw>7) afectaron a este área en los últimos 7000 años. El periodo de recurrencia de estos eventos catastróficos se ha calculado entre 1200 y 1500 años.Publicación Procesos cársticos en terrazas marinas del último interglaciar asociados a cambios climáticos y de nivel del mar (Golfo de Cádiz, España)(AEQUA, 2005) Cabero, Ana; Zazo Cardeña, Caridad; Goy Goy, José Luis; Dabrio, Cristino José; Borja, Francisco; Bardají Azcárate, Teresa; Silva, Pablo Gabriel; Roquero García-Casal, Elvira; Lario Gómez, JavierThe coastal strip between Trafalgar and Punta Paloma, is characterized by the development of a karstic complex that affects the Last Interglacial marine terraces (OIS 5c ~100 ka, Fig. 1), there composed of well cemented conglomerates and sandstones. Two different morphologies are recorded, both related to different genetic models: "solution pipes" controlled by climatic changes (switch from humidity to aridity), and "horizontal tubules" controlled by changes in base level. The origin and palaeoenvironmental meaning of these karstic forms are described for the first time in the littoral of Cadiz, within a chronological framework based on OSL (Optically Stimulated Luminescence) and U/Th (alpha and TIMS) dating.Publicación The coastal record of tsunamis in the INQUA ESI-2007 scale(Instituto Geológico y Minero de España, 2014) Bardají Azcárate, Teresa; Silva, Pablo Gabriel; Zazo Cardeña, Caridad; Goy Goy, José Luis; Cabero, Ana; Lario Gómez, JavierSeismic Intensity scales are based on the effects of earthquakes on man, man-made structures and on natural environment. However, the effects on the environment have been usually minimized because they were considered as inaccurate features. The growth of Palaeoseismology as an independent discipline led to the development of the ESI-2007 Intensity Scale, based on the effects of earthquakes on the environment and ratified by INQUA during its XVII Congress (Cairns, Australia-2007). This scale can be used alone or jointly with other intensity scales, but it becomes especially useful for seismic intensity higher than X, when damage-based scales get saturated and environmental effects are still diagnostic. Tsunamis are only considered in the ESI-scale by the height of the waves, and no by their geological or sedimentary record. Data from present day tsunamis (authors’ own work and other’s published data) are used as a first approach to the implementation of this record in the ESI-scale. However, the joint effort of an international working group is desirable in order to properly match effects and intensity degrees.Publicación The record of highstand sea-level during the Iast interglacials (Isotope Stages 7, 5 and 1) in the Atlantic-Mediterranean linkage area(Gibraltar Govemment Heritage Division, 2000) Zazo Cardeña, Caridad; Goy Goy, José Luis; Hillaire Marcel, Claude; Dabrio, Cristino José; Hoyos Gómez, Manuel; Bardají Azcárate, Teresa; Silva, Pablo Gabriel; Somoza, L.; Lario Gómez, Javier