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  • 1
    Electronic Resource
    Electronic Resource
    Springer
    International journal of earth sciences 73 (1984), S. 577-598 
    ISSN: 1437-3262
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Description / Table of Contents: Abstract The Mesozoic lavas and minor intrusions in the thrust sheets of western Sicily have the following characteristics: 1. The lavas in the Triassic Mufara Formation in the north were broken into fragments which rotated independently within the incompetent strata that enclose them. This behavior is characteristic of igneous rocks found within the more internal (northerly) thrust units. 2. The Jurassic lavas in the more external (southerly) units have consistent directions which agree with those of the Ammonitico Rosso limestones in the same zone and lie about 30° clockwise from those of coeval autochthonous formations in Tunisia.Schult's presumed Cretaceous directions from Custonaci on the north coast (similar to those found in the Cretaceous Scaglia Rossa at Terrasini to the east byChannel et al., 1980) are rotated still more (140°) with respect to those of the autochthonous Iblean platform of SE Sicily. These differences are believed to reflect rotation of the thrust sheets during tectonic transport in Cenozoic times, the internal units being the most strongly rotated. 3. All the igneous rocks are highly altered: generally the original mineralogy cannot be completely determined. Relative abundances of some of the less mobile elements (Ti, Sr, Y) suggest that they are intraplate basalts.
    Abstract: Résumé Les laves et les instrusions mineures mésozoïques présentes dans les roches charriées de la Sicile occidentale montrent les caractéristiques suivantes: 1. Les laves intercalées dans la Formation de Mufara d'âge triasique ont été morcelées en fragments qui ont subi des rotations indépendantes dans les marnes incompétentes qui les enrobent. Ce comportement est typique des roches ignées qui se trouvent dans les unités charriées de la zone plus interne (septentrionale). 2. Les laves jurassiques des unités plus externes (méridionales) possèdent des directions d'aimantation qui accordenz avec celles des calcaires de l'ammonitico rosso de la même zone externe qui déviées d'environ 30° vers la droite par rapport aux roches de même âge de la Tunisie. Les directions, dites crétacées de Schult, de la région de Custonaci sur la côte septentrionale (qui concordent bien avec celles trouvées parChannell et al. (1980) à Terrasini) différent encore plus, avec une rotation de 140°, par rapport à la plateforme autochtone d'Iblei (Sicile) SE). Ces différences sont interprétées comme reflétant la rotation des nappes charriées au cours du transport tectonique durant le Cenozoïque, la zone interne ayant subi une rotation plus intense. 3. Toutes les roches ignées sont fortement altérées; en général on ne peut pas identifier les minéraux originels. L'abondance relative de certains des éléments non-mobiles (Ti, Sr, Y) suggèrent une origine intracratonique.
    Notes: Zusammenfassung Die mesozoischen Laven und kleineren Intrusionen innerhalb der Schuppen von Westsizilien besitzen folgende Charakteristika: 1. Die Laven innerhalb der triassischen Mufara-Formation im Norden sind zerbrochen zu Fragmenten, die unabhängig voneinander innerhalb der umgebenden inkompetenten Schichten rotiert wurden. Dieses ist für die magmatischen Gesteine der inneren (nördlicheren) Überschiebungseinheiten typisch. 2. Die jurassischen Laven der externeren (südlicheren) Einheiten besitzen übereinstimmende Richtungen, die mit denen der Ammonitico-Rosso-Kalke derselben Zone übereinstimmen. Diese liegen um etwa 30° im Uhrzeigersinn verdreht gegenüber den Richtungen der gleich alten autochthonen Formation in Tunesien. Die vonSchult angenommenen kretazischen Richtungen von Custonaci an der Nordküste (ähnlich denen aus der kretazischen Scaglia Rossa von Terrasini) im Osten (beschrieben vonChannel et al., 1980) sind noch weiter rotiert (140°), bezogen auf die der autochthonen Plattform von Iblea im SE Siziliens. Es wird angenommen, daß diese Differenzen eine Drehung der überschobenen Einheiten während des tektonischen Transportes in känozoischer Zeit abbilden. Die inneren Einheiten wurden dabei am stärksten rotiert. 3. Alle magmatischen Steine sind hochgradig alteriert. Die Ausgangszusammensetzung der Gesteine kann generell nicht mehr vollständig bestimmt werden. Die relative Häufigkeit einiger der wenigen mobilen Elemente (Ti, Sr, Y) läßt sie als Intraplatten- Basalte vermuten.
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Histochemistry and cell biology 40 (1974), S. 129-135 
    ISSN: 1432-119X
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Medicine
    Notes: Summary Mast cells of the Mongolian gerbil Meriones unguiculatus, the hog Sus scrofa, the cat Felis catus and the armadillo Pasypus novemcinctus were studied histochemically in relation to various fixation procedures, using azure A at pH 1 and 3, alcian blue at pH 1 and 2.5, diazosafranin at pH 3 and 7.8–8, and the PAS reaction. Fixations were performed in buffered 10% formol and 5% glutaraldehyde, in Kose's fluid, buffered sublimate (B4), lead nitrate and lead acetate formol. With azure A and alcian blue many mast cells were found in the gerbil with the aldehyde fixatives, fewer with the heavy metals. The diazosafranin reaction was present only in the aldehyde material, the PAS reaction was negative. In the hog, mast cells were more numerous after heavy metal fixation, fewer with aldehydes. Azure A stained metachromatically at pH 1 and 3, alcian blue reacted only at pH 1, the PAS reaction was negative, the pH 3 and 8 diazosafranin reactions were positive with all 4 fixations. In the cat, mast cells were moderately numerous with lead acetate formol, rare with formol and absent with glutaraldehyde. They stained with azure A at pH 1 and 3, with alcian blue at pH 1 and 2.5, with diazosafranin at pH 3 and 8 and by the PAS reaction. Armadillo mast cells were more numerous after heavy metal fixations, stained with azure A and alcian blue at pH 1 and 2.5 to 3, and with acid and alkaline diazosafranin. The mast cells of the 4 species vary in their requirements for aldehyde and heavy metal fixation, in their PAS reactivity and in their pH 2.5 alcian blue staining. All are sufficiently sulfated to react to cationic dyes at pH 1, but vary in PAS reactivity, indicating partial or complete sulfation. The presence of 5-hydroxytryptamine is indicated in all four species.
    Type of Medium: Electronic Resource
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  • 3
    Publication Date: 2017-04-04
    Description: Tritium is a naturally occurring radionuclide, due to interactions of cosmic-rays with the upper layers of the atmosphere; but its presence in the environment is mainly due to residual fallout from nuclear weapons atmosphere tests, carried out from 1952 till 1980. Tritium reaches the Earth’s surface mainly in the form of precipitation, becoming part of the hydrological cycle, then the interest of tritium content analysis in drinking water is both for dosimetry and health-risk and for using tritium as a natural tracer in the groundwater circulation system. This paper presents results from a survey carried out in the Mt. Etna area (east and west flanks) and in the southern side of Nebrodi in Sicily (Italy), in order to determine tritium activity concentrations in water samples by using liquid scintillation counter. The investigated areas show quite low tritium concentrations, much below the Italian limit of 100 Bq L-1 for drinking water and even comparable with the minimum detectable activity value. The effective dose due to tritium for public drinking water consumption was also evaluated.
    Description: Published
    Description: 861-866
    Description: 6A. Monitoraggio ambientale, sicurezza e territorio
    Description: JCR Journal
    Description: restricted
    Keywords: Tritium ; Tritiated water ; Liquid scintillation ; Mt. Etna ; Drinking water ; 03. Hydrosphere::03.04. Chemical and biological::03.04.07. Radioactivity and isotopes
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 4
    Publication Date: 2013-08-30
    Print ISSN: 0236-5731
    Electronic ISSN: 1588-2780
    Topics: Chemistry and Pharmacology , Energy, Environment Protection, Nuclear Power Engineering
    Published by Springer
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  • 5
    Publication Date: 2016-10-15
    Description: New observations on the Sicily Messinian Tripoli have yielded a variably thick diatomitic, calcareous and shaly rock interval marked by an upwards disappearance of calcareous and siliceous plankton (barren lithosome), coexisting with a variability in vegetal remains and significant amounts of amorphous organic matter (AOM). Facies analysis associated with biostratigraphy and palaeoecology of the several field and borehole sections has been framed in a well-accepted chronological scheme that points to this barren interval coinciding with the stratigraphic upper and younger part of some Tripoli sections (bituminous Tripoli) located in the northern part of the study area. Biostratigraphically, the barren lithosome falls within the Non-Distinctive Zone (NDZ) and is generally younger than the First Common Occurrence (FCO) of T . multiloba . The age of its diachronous base appears older than the Messinian salinity crisis (MSC) deposits, because is well constrained by the calcareous plankton biostratigraphic markers along the underlying portions of the Tripoli. The top boundary of the barren rock interval, that is not always identifiable, could be age dated, following the proposed stratigraphic criteria. We infer that the Tripoli initial open-marine environment became, in more inner areas, progressively confined, with freshwater floodings alternating with short marine-water incursions in a shallow-water to continental domain. The collected information appears useful in addressing further exploration.
    Print ISSN: 1354-0793
    Topics: Chemistry and Pharmacology , Geosciences
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  • 6
    Publication Date: 2014-03-08
    Description: The study of geological evolution of a multiphase orogenic belt is complex, expecially when the tectonic events are superimposed in a coaxial fashion. The Sicilian fold-and-thrust belt represents an interesting case study, as a non-coaxial superimposition of structures is recognizable, owing to large synkinematic clockwise rotations during each of two subsequent compressional events. These rotations involved also the syntectonic basins that developed in the wedge-top depozone. This study aims to constrain the tectono-depositional evolution of the NW Sicily fold-and-thrust belt and the associated wedge-top depozone between the middle Miocene and the early Pliocene. Integrated analyses of stratigraphic, sedimentological and structural field data allow us to better constrain the transition between the two tectonic events. The syntectonic basins developed during the first (late Serravallian–early Tortonian) tectonic event were relatively wide and characterized by marine sedimentation. The onset of the second (latest Tortonian) transpressional event induced localized deformation into the wedge-top depozone and the syntectonic successions were accommodated as basin fill in progressively narrower and laterally discontinuous basins, bounded by transpressional structures. The lateral correlation of the wedge-top successions suggests a latest Miocene regional palaeoslope with a present-day WSW dip, which fits well with the tectonic transport calculated for the early compressional event.
    Print ISSN: 0016-7649
    Topics: Geosciences
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  • 7
    Publication Date: 2013-05-08
    Description: Sicily is a thick orogenic wedge formed by (1) the foreland (African) and its Sicilian orogen and (2) the thick-skinned, Calabrian–Peloritani wedge. The crust under central Sicily, from the Tyrrhenian margin to the coastline of the Sicily Channel, has been investigated by the multidisciplinary (SI.RI.PRO.) research project. The project dealt with the nature and thickness of the crust and depth and geometry of the Moho, which is essential in formulating subduction models and improving the knowledge of African and Tyrrhenian–European lithospheres. The results resolve features such as (1) the main orogenic wedge, (2) the very steep, NW–SE-trending regional monocline suggesting inflection of the foreland crust, (3) the deep Caltanissetta synform imaged, for the first time, to about 25 km, and (4) the top of the crystalline basement and the inferred crust–mantle boundary. The SI.RI.PRO. transect confirmed that the NNW-dipping, autochthonous Iblean platform of SE Sicily and its basement extends all the way into central Sicily. Further NW, towards the NNW end of the transect, a large uplift involves the Iblean platform and its underlying basement. The associated gravity anomaly is interpreted as the southern wedge edge of the Tyrrhenian mantle that splits the subducting Iblean–Pelagian (African) continental slab from an overlying synformal stack of allochthonous thrust sheets. Supplementary materials: Additional data are available at www.geolsoc.org.uk/SUP18594 .
    Print ISSN: 0016-7649
    Topics: Geosciences
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  • 8
  • 9
    Publication Date: 2015-05-01
    Print ISSN: 1951-6355
    Electronic ISSN: 1951-6401
    Topics: Physics
    Published by Springer
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  • 10
    Publication Date: 2008-04-25
    Print ISSN: 1434-6060
    Electronic ISSN: 1434-6079
    Topics: Physics
    Published by Springer
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