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  • 1
    Publication Date: 2017-04-04
    Description: The November 12, 1999, Mw 7.1 earthquake, ruptured the Düzce segment of the North Anatolian Fault Zone and produced ca. 40 km-long surface ruptures. To learn about recurrence of large surface faulting earthquakes on this fault, we undertook paleoseismological trench investigations. We found evidence for repeated surface faulting paleoearthquakes pre-dating the 1999 event. Dating was based on radiocarbon and 210Pb analyses as well as on archaeological considerations. By merging information obtained from all the trenches we reconstructed the seismic history of the Düzce fault for the past millennium. We correlated coeval events between different trench sites under the assumption that, similarly to the 1999 event, paleoearthquakes ruptured the whole Düzce fault. Besides the 1999 earthquake, prior surface faulting earthquakes are dated as follows: AD1685-1900 (possibly end of 19th century); AD1685-1900 (possibly close to AD 1700); AD1185-1640; AD685-1220 (possibly AD800-1000). Thus, the AD1719, AD1878 and AD1894 historical earthquakes, may have ruptured the Düzce fault and not the faults they are usually associated to or, alternatively, a cascade of events occurred on the Düzce and nearby faults (similarly to the Izmit and Düzce 1999 earthquakes). Five events since AD 685-1220 (possibly AD800-1000), would yield an average recurrence time for the Düzce fault, of 200-325 yr (possibly 250-300 yr). The three most recent earthquakes, including 1999, occurred within 300 yr and may be suggestive of clustering. Assuming that the average 1999 slip is characteristic for this fault, the above recurrence times yield slip rates of 6.7-13.5 mm/yr.
    Description: E.C. project Relief (EVG1-CT-2002-00069)
    Description: Submitted
    Description: open
    Keywords: 1999 Duzce earthquake ; paleoseismicity ; earthquake recurrence ; 04. Solid Earth::04.04. Geology::04.04.01. Earthquake geology and paleoseismology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: manuscript
    Format: 8843563 bytes
    Format: 10358162 bytes
    Format: 8600598 bytes
    Format: application/pdf
    Format: application/pdf
    Format: application/pdf
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  • 2
    Publication Date: 2017-04-04
    Description: 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.
    Description: Published
    Description: 37-49
    Description: 3.3. Geodinamica e struttura dell'interno della Terra
    Description: N/A or not JCR
    Description: reserved
    Keywords: 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)
    Type: article
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  • 3
    Publication Date: 2017-04-04
    Description: The November 12, 1999, Mw 7.1 earthquake, ruptured the Düzce segment of the North Anatolian Fault Zone and produced a ca. 40 km-long surface rupture. To improve knowledge about earthquake recurrence on this fault, we undertook paleoseismological trench investigations. We found evidence for repeated surface faulting paleoearthquakes pre-dating the 1999 event during the past millennium. Dating was based on radiocarbon, 210Pb analyses, and archaeological considerations. In addition to the 1999 earthquake, prior surface faulting earthquakes are dated as follows: AD1685-1900 (possibly end of 19th century); AD1495-1700; AD685-1020 (possibly AD890-1020). The AD967 and AD1878 historical earthquakes are good candidates to have ruptured the Düzce fault correlating with the oldest and penultimate paleoearthquakes. No obvious correlation for the third paleoearthquake (AD1495-1700) exists. These results shows that the Düzce fault considerably participates, along with the parallel Mudurnu fault sections, in the seismogenic deformation taking place along this part of the North Anatolian Fault. Four events since AD 685-1020 (possibly AD890-1020), would yield an average recurrence time for the Düzce fault of 330-430 yr (possibly 330-370 yr). The three most recent earthquakes, including 1999, occurred within 500 yr. Merging results from other paleoseismological studies along the Düzce fault show a consistency of results and yields average recurrence times for the past 2000 yr of 320-390 yr. Assuming that the 1999 slip (2.7 m average, 5 m maximum) is representative of the behavior of this fault, the above recurrence times yield a reference figure of fault slip rate in the range 6.9-15.6 mm/yr.
    Description: European Community project RELIEF
    Description: In press
    Description: 3.2. Tettonica attiva
    Description: JCR Journal
    Description: open
    Keywords: 1999 earthquake ; North Anatolian Fault ; Paleoearthquakes ; earthquake recurrence ; 04. Solid Earth::04.04. Geology::04.04.01. Earthquake geology and paleoseismology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: manuscript
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  • 4
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    Unknown
    Université de Provence, conseil régional PACA, CNRS, TELEMME, CEREGE, Université Federico Due de Naples
    Publication Date: 2019-12-18
    Description: Historical sources testify to the flourishing maritime activity at the ancient town of Tindari, mentioning a harbour but not supplying information on its location, size or configuration. Because a town as important as Tindari must have had a landing place for ships, we examined new sources of information with the aim to localize traces of the harbour. Holocene uplifted and submerged notches, identified along the Tindari promontory, and the mooring iron rings, testify to past sea level changes. These elements are used to reconstruct the palaeotopography of Tindari Cape and the Oliveri coastal plain in the 4th century BC. The reconstruction reveals a safe landing place southeast of the Tindari Cape suitably protected from prevailing winds.
    Description: Published
    Description: 69-74
    Description: 3.3. Geodinamica e struttura dell'interno della Terra
    Description: N/A or not JCR
    Description: reserved
    Keywords: geoarchaeology ; Tindari ; harbour ; digital terrain model ; Sicily ; Italy ; 04. Solid Earth::04.01. Earth Interior::04.01.99. General or miscellaneous ; 04. Solid Earth::04.07. Tectonophysics::04.07.99. General or miscellaneous ; 04. Solid Earth::04.07. Tectonophysics::04.07.02. Geodynamics
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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