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Fault and basin depocentre migration over the last 2 Ma in the L'Aquila 2009 earthquake region, central Italian Apennines
Abstract Morphological, stratigraphical and structural investigations integrated with palaeomagnetic and tephrostratigraphic studies and 40 Ar/ 39 Ar measurements allowed us to define the QuaternaryExpand
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Mid-distal occurrences of the Albano Maar pyroclastic deposits and their relevance for reassessing the eruptive scenarios of the most recent activity at the Colli Albani Volcanic District, Central
Abstract The Late Pleistocene Albano Maar hosted the most recent volcanic activity of the Colli Albani Volcanic District, represented at near-vent sections by a thick pyroclastic succession of sevenExpand
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40Ar/39Ar and 14C geochronology of the Albano maar deposits: Implications for defining the age and eruptive style of the most recent explosive activity at Colli Albani Volcanic District, Central Italy
Abstract New 40 Ar/ 39 Ar and 14 C ages have been found for the Albano multiple maar pyroclastic units and underlying paleosols to document the most recent explosive activity in the Colli AlbaniExpand
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Marine geological and archaeological evidence of a possible pre-Neolithic site in Pantelleria Island, Central Mediterranean Sea
Abstract Recent underwater archaeological surveys recovered hundreds of flint artefacts between depths of 18 and 21 m at Cala Tramontana, a small bay located in the eastern part of PantelleriaExpand
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Tephra layers from Holocene lake sediments of the Sulmona basin, central Italy: implications for volcanic activity in Peninsular Italy and tephrostratigraphy in the central Mediterranean area
Abstract We present a new tephrostratigraphic record from the Holocene lake sediments of the Sulmona basin, central Italy. The Holocene succession is represented by whitish calcareous mud that isExpand
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Structure and evolution of the Sacrofano-Baccano caldera, Sabatini volcanic complex, Rome
Abstract Sacrofano eruptive center, in the eastern part of the Sabatini volcanic complex, was active between 0.5 and 0.09 m.y. ago. The Baccano geothermal area lies at the western edge of SacrofanoExpand
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