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  • 04. Solid Earth::04.07. Tectonophysics::04.07.02. Geodynamics  (4)
  • Agu  (1)
  • Association for Environmental Archaeology - Maney  (1)
  • Blackwell Publishing Ltd  (1)
  • Istituto Nazionale di Geofisica e Vulcanologia - TU Berlin  (1)
  • Annual Reviews
  • 2005-2009  (4)
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  • 2005-2009  (4)
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  • 1
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    Istituto Nazionale di Geofisica e Vulcanologia - TU Berlin
    Publikationsdatum: 2017-04-04
    Beschreibung: A short review of the more relevant modern arguments in favour of the conception of the Earth in expansion is provided. The advantage of the expanding planet idea is a common explanation of several outstanding problems coming from palaeontology, palaeomagnetism, geology and climatology. All these problems should be regarded as be a sort of distortion effects, which arise if we try to reconstruct the situation of old geologic times adopting the modern Earth’s radius – the distortions become larger and larger as we came back in time. As a consequence the expanding Earth could be considered a natural generalization of the plate tectonic. A strong support to this generalization came from the simple and united explanation that can be found in the expanding Earth of the classical geodynamic phenomena of the polar motion and the true polar wander by an inversion of the paleogeographic position of the triple points. The conviction is expressed that basic information about this old global tectonic conception should be provided in secondary school and university courses.
    Beschreibung: Published
    Beschreibung: 181-232
    Beschreibung: open
    Schlagwort(e): Global tectonics, geodynamics ; paleogeography, expanding Earth ; 04. Solid Earth::04.01. Earth Interior::04.01.02. Geological and geophysical evidences of deep processes ; 04. Solid Earth::04.03. Geodesy::04.03.02. Earth rotation ; 04. Solid Earth::04.07. Tectonophysics::04.07.02. Geodynamics ; 04. Solid Earth::04.07. Tectonophysics::04.07.04. Plate boundaries, motion, and tectonics
    Repository-Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Materialart: book chapter
    Format: 1871163 bytes
    Format: application/pdf
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 2
    Publikationsdatum: 2017-04-04
    Beschreibung: New seismological and structural data from the central Adriatic-Gargano promontory area demonstrate that the current models of an aseismic and slightly deformed Adriatic block have to be revised. A seismically active deformational belt is mapped along two main fault systems, the Tremiti Islands and Mattinata faults. Moreover, geologic and geophysical evidence suggests that a more extensive lithospheric boundary may cut across the central Italian peninsula to the Tyrrhenian basin.
    Beschreibung: Published
    Beschreibung: 109-117
    Beschreibung: JCR Journal
    Beschreibung: open
    Schlagwort(e): Adriatic Sea ; Geodynamics ; 04. Solid Earth::04.07. Tectonophysics::04.07.02. Geodynamics
    Repository-Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Materialart: article
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 3
    Publikationsdatum: 2017-04-04
    Beschreibung: In the Greek and Roman periods, the fortified town of Tindari’s military and trading importance combined with its strategic location in north-east Sicily allowed it to control traffic on the Tyrrhenian Sea for many centuries. Historical sources (Polybius, Cicero, Livy and Appian) testify to the flourishing maritime activity of the ancient town, but do not supply any information on the location, size or configuration of its harbour. Because a town as important as Tindari must have had a landing place for ships, we examined new sources of information with the aim of identifying its location. Historiographical and archaeological surveys produced evidence of a well-organised harbour. Geomorphological investigations, performed along the Tindari Promontory, identified Holocene uplifted and submerged notches indicating past sea level changes. Furthermore, it was found that in the last four centuries the combined actions of marine and fluvial dynamics had produced a progressive filling of the Oliveri lowland and a progradation of the shoreline, which was responsible for the burial of ancient buildings. The palaeotopographic reconstruction of the Tindari Cape Promontory and Oliveri coastal plain in the 4th century BC shows a safe landing place south-east of the Tindari Cape that was suitably protected from prevailing winds.
    Beschreibung: Published
    Beschreibung: 37-49
    Beschreibung: 3.3. Geodinamica e struttura dell'interno della Terra
    Beschreibung: N/A or not JCR
    Beschreibung: reserved
    Schlagwort(e): geoarchaeology ; Tindari harbour ; marine notches ; paleotopographic reconstruction ; 04. Solid Earth::04.07. Tectonophysics::04.07.02. Geodynamics
    Repository-Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Materialart: article
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 4
    Publikationsdatum: 2012-02-03
    Beschreibung: We analyse P-wave traveltimes for the Mediterranean area, using both teleseismic and regional arrivals for shallow earthquakes reported in the Bulletins of the International Seismological Centre. We model delays between pairs of 0.5° × 0.5° cells, obtaining a detailed representation of the P traveltime heterogeneities. Examination of these anomalies shows the clear presence of geographically coherent patterns—consistent with known geological features—due to significant structure in the upper mantle. We present a scheme, based on an empirical heterogeneity correction (EHC) to P-wave traveltimes, to improve earthquake location. This method provides similar benefits to those of a location procedure based on ray tracing in a 3-D model, but it is simpler and computationally more efficient. The definition of the traveltime heterogeneity model, being based on a statistical procedure, bypasses most of the critical points and possible instabilities involved in model inversion. EHC relocation, applied to Mediterranean earthquakes, allows one to predict about 70 per cent of the estimated signal due to heterogeneity and produces epicentral and origin time-shifts of, respectively, 4.22 km and 0.35 s (rms). From a synthetic experiment, in which we use the proposed algorithm to retrieve known source locations, we estimate that the rms improvement achieved by the EHC relocation over a simpler, standard, 1-D location is more than 20 per cent for both epicentral mislocation and origin time-shifts.
    Beschreibung: Published
    Beschreibung: 232-254
    Beschreibung: 3.3. Geodinamica e struttura dell'interno della Terra
    Beschreibung: JCR Journal
    Beschreibung: reserved
    Schlagwort(e): earthquake location ; Mediterranean ; P waves ; traveltime ; upper mantle ; 04. Solid Earth::04.07. Tectonophysics::04.07.02. Geodynamics
    Repository-Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Materialart: article
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
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