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  • crustal deformations  (5)
  • 1
    Publication Date: 2017-04-04
    Description: Th Messina Straits (southern Italy) on December 28, 1908 was struck by a Ms=7.5, seismic event, that was the largest earthquake occurred in Italy during the last 100 years. The earthquake and the related tsunami caused thousands of victims and severe destruction in a wide area along the Sicilian and Calabrian coasts. After that time many geophysical and geological studies were developed to evaluate the seismic characteristics of the 1908 earthquake, the seismic risk and the geological evolution of the region in the framework of the Mediterranean geodynamics, characterized by the collision between the African and Eurasian plates. With the aim to evaluate the present crustal motion of this area, that undergone a recent tectonic evolution that produced an important uplift during the last 125 Kyears, since 1970 was started a geodetic research. A geodetic network was set up across the Straits and repeatedly measured with terrestrial techniques till 1980. In 1987, a 7 vertices network (4 vertices in common with the already existent network) was surveyed for the first time by the GPS space technique, improving the accuracy of the coordinate determinations. Finally, in 1994 a wider network was established and surveyed again to collect additional GPS observations about a larger area across the Straits. In this paper we provide a general geophysical description of the Area and the results obtained by the analysis of two GPS surveys (1987 and 1994) with respect to those achieved by the terrestrial surveys (from 1970 to 1980). Our analysis leads to exclude the occurrence of significant crustal horizontal deformations across the Straits in ha last 15 years; this conclusion is in agreement with current geophysical models that exclude any aseismic deformations acting in this area.
    Description: Published
    Description: 3-14
    Description: 1.1. TTC - Monitoraggio sismico del territorio nazionale
    Description: N/A or not JCR
    Description: open
    Keywords: Messina Straits ; crustal deformations ; terrestrial and GPS surveys ; gravimetry ; 04. Solid Earth::04.03. Geodesy::04.03.01. Crustal deformations
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2017-04-04
    Description: In this paper we present the GPS data collected at 18 stations of the IGM95 GPS network, in the colfiorito and Sellano areas. The data show ground deformations due to the largest earthquakes of the umbria-marche seismic sequence of September-October, 1997. The first two events, occurred on September 26, Mw=5.7 and Mw=6.0, produced planoaltimetric displacements up to 25 cm in the Colfiorito area. The October 14, 1997 earthquake, occurred near Sellano village and produced visible ground deformations that were not revealed at the GPS monuments dut to the unfavorable GPS IGM95 network configuration in this area. We present and discuss the whole geodetic data set collected in the area, useful to update the 3-D coordinates of the IGM95 GPS monuments, for scientific and civil applications.
    Description: Published
    Description: 281-290
    Description: 1.1. TTC - Monitoraggio sismico del territorio nazionale
    Description: N/A or not JCR
    Description: open
    Keywords: Earthquakes ; crustal deformations ; GPS ; IGM95 Network ; 04. Solid Earth::04.03. Geodesy::04.03.07. Satellite geodesy
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 3
    Publication Date: 2020-02-24
    Description: The TYRGEONET project was born from the cooperation of many Italian and foreign Institutions to monitor crustal deformations in the Central Mediterranean area by spatial techniques.
    Description: Published
    Description: 251-255
    Description: 3.3. Geodinamica e struttura dell'interno della Terra
    Description: N/A or not JCR
    Description: restricted
    Keywords: crustal deformations ; GPS ; 04. Solid Earth::04.03. Geodesy::04.03.01. Crustal deformations
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 4
    Publication Date: 2019-11-04
    Description: The area located between Catania and Syracuse (Southeastern Sicily), characterised by the presence of the Simeto-Scordia-Lentini graben, was affected in the past by a strong seismicity as proved by the occurrence of seismic events strong enough to reach the XI degree of the MCS scale. In particular the January 11 th, 1693 (l = XI MCS) earthquake with a magnitude over 7.5 (estimated), caused huge damage and a great loss of human lives. Following the last seismic event which occurred on December 13th, 1990 (Ml = 5.4) which caused heavy damage and many victims in the Catania-Syracuse area, a geodetic Global Positioning System network (GPS) was set up with the aim of monitoring ground movements in one of the Italian areas subjected to high seismic risk, This "pace geodesy technique supplies high precision measurements and represent, a powerful new tool for investigating both regional stress fields and the evolution of local tectonic areas. The GPS network will allow the detection of ground movements with a centimetric accuracy through repeated surveys in time. The results obtained in two surveys carried out il1 1991 al1d 1993, are described in this paper.
    Description: JCR Journal
    Description: open
    Keywords: Global Positioning System (GPS) ; crustal deformations ; 04. Solid Earth::04.03. Geodesy::04.03.99. General or miscellaneous ; 04. Solid Earth::04.03. Geodesy::04.03.01. Crustal deformations
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Format: 2903657 bytes
    Format: application/pdf
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  • 5
    Publication Date: 2019-11-04
    Description: Geodetic and seismic evidence of crustal deformations in the Ionian area are shown in this paper. The Ionian GPS network, composed of nine sites crossing the Ionian Sea from Calabria, Southern Italy, to Northwestern Greece, was established and surveyed in 1991, 1994, 1995 within the framework of the TYRGEONET project (Anzidei et al., 1996). In 1996 a return campaign was carried out after the occurrence of seismic activity in 1995. The displacement pattern obtained for the Greek side of the network agrees well with those previously displayed, both in magnitude and direction, confirming a mean displacement rate of about 1-2 cm1/yr. The same agreement is not found for the Italian side of the network, where no significant deformations were detected between 1994 and 1996. Seismic deformation was also studied for the same area, starting from the moment tensors of events which occurred in the last 20 years with magnitude greater than 5.0; evident similarity with the displacement field exhibited by the Greek side of the Ionian Sea by geodetic surveys was inferred. On the contrary, the motion detected for the Italian area cannot be simply related to seismic activity.
    Description: JCR Journal
    Description: open
    Keywords: GPS ; crustal deformations ; seismicity ; Ionian Sea ; 04. Solid Earth::04.02. Exploration geophysics::04.02.05. Downhole, radioactivity, remote sensing, and other methods ; 04. Solid Earth::04.03. Geodesy::04.03.01. Crustal deformations
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Format: 4283799 bytes
    Format: application/pdf
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