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  • Natural radioactivity  (1)
  • new evidence for calc-alkaline explosive volcanism in the Southern Tyrrhenian Sea  (1)
  • tectonic setting of triassic magmatism  (1)
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  • 1
    Publikationsdatum: 2018-04-26
    Beschreibung: Petrological and geochemical data of Triassic magmatic rocks from Lercara Basin (Central Sicily), provide new information about the intraplate volcanism related to the Pangea break up. The magmatic rocks crop out as subvolcanic bodies and are packed in several Lower Triassic clayey lithologies correlated to the sedimentation inside the Imerese and Sicano domains. The samples are splitted in two groups: the first includes transitional to alkaline basalts, with sub-ophitic texture; the second includes more altered rocks, with porphyritic texture, showing alkali basaltic to phonolitic compositions. Major and trace element data of single groups show small variations indicating fractional crystallization processes. Abundances and ratios of incompatible trace elements indicate that rocks were formed in an intraplate continental environment from different mantle sources with E-MORB to OIB-type compositions. Low partial melting degrees at the transition between spinel and garnet lherzolite fields can be hypothesized for parental magmas of the Lercara Basin. We propose that magma batches moved toward the surface along lithospheric fractures originated by flexure and uplift of the Mesozoic Pangea supercontinent.
    Beschreibung: Published
    Beschreibung: 169-181
    Beschreibung: 2V. Struttura e sistema di alimentazione dei vulcani
    Beschreibung: JCR Journal
    Schlagwort(e): intraplate continental volcanism ; spinel-garnet-lherzolite source ; tectonic setting of triassic magmatism
    Repository-Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Materialart: article
    Standort Signatur Erwartet Verfügbarkeit
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  • 2
    Publikationsdatum: 2018-04-11
    Beschreibung: A well-preserved volcaniclastic sequence crops out in Pleistocene marine sediments along the Tyrrhenian coastline of the Calabrian-Peloritani arc (Sicily, Italy), testifying the occurrence of Lower-Middle Pleistocene volcanic activity in Southern Tyrrhenian Sea. The presence of dominant highly vesicular and minor blocky glassy particles indicates that the volcanic clasts were originated by explosive events related to the ascent and violent emission of volatile-rich magmas accompanied by and/or alternated with hydromagmatic fragmentation due to magma-sea water interaction. Field investigations and sedimentological features of the studied volcaniclastic units suggest a deposition from sediment-water density 􀃀ows. The chemical classi􀂿cation of the pumice clasts indicates prevalent rhyolitic and dacitic compositions with calc-alkaline to high-K calc-alkaline af􀂿nity. The geochemical features of immobile trace elements together with the presence of orthopyroxene are indicative of a provenance from an arc-type environment. The age (from 980-910 to 589 ka), the chemical composition and the evidence of subaerial explosive volcanic activity constrain the origin nature and temporal evolution of the arc-type volcanism in the Southern Tyrrhenian domain. Finally, the new information here provided contribute to a better understanding of the temporal geodynamic evolution of this sector of the Mediterranean domain.
    Beschreibung: Published
    Beschreibung: 371-389
    Beschreibung: 1V. Storia eruttiva
    Beschreibung: JCR Journal
    Schlagwort(e): volcaniclastic deposits ; Pleistocene volcanism ; new evidence for calc-alkaline explosive volcanism in the Southern Tyrrhenian Sea
    Repository-Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Materialart: article
    Standort Signatur Erwartet Verfügbarkeit
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  • 3
    Publikationsdatum: 2024-05-16
    Beschreibung: Radon measurements in soil gases were carried out along the Tyrrhenian margin of north-eastern Sicily (southern Apennines of Italy), one of the most tectonically and seismically active areas within the central Mediterranean region. The collected data highlight an ~ NW–SE oriented zone located to the south of the Milazzo Peninsula marked by intense soil radon degassing. Concentrations of 222Rn and 220Rn were derived to be in the range of 0.69–81.3 kBq m− 3 and 2.63–123.48 kBq m− 3, respectively. The widespread radon release seems to be induced by the uprising of deep-originated fluids along faults and joints, and it is favoured by the high permeability of the outcropping alluvial Quaternary sediments. Moreover, the potential tectonic structure promoting the soil radon degassing may act as the “silent” on-land prolongation of the Vulcano-Milazzo fault zone (VMFZ), a transtensional tectonic element located in the Gulf of Patti and belonging to the Aeolian–Tindari– Letojanni System (ATLFS). The collected results are in accordance with previous studies showing the close relationship between regional degassing and tectonic activity. Periodical and continuous monitoring of radon emission over the area is considered of basic importance to better assess the radiological/health hazard for the population, which in this study was primarily evaluated from low to moderate in terms of first-level screening, as well as in view of possible development of the seismogenic process that can intensify the releasing of endogenous fluids.
    Beschreibung: Published
    Beschreibung: 273
    Beschreibung: JCR Journal
    Schlagwort(e): Natural radioactivity ; Soil radon degassing ; Radiological hazard ; Deep-originated volatiles
    Repository-Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Materialart: article
    Standort Signatur Erwartet Verfügbarkeit
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