In 2010 and 2015 two geophysical surveys were carried out in the Tyrrhenian basin withinthe framework of a Spanish-German-Italian projects MEDOC and the CHIANTI, respectively.During the MEDoC survey a total of 17 Multichannel seismic (MCS) lines for a total length of2.808 km and 5 long Wide-Angle Seismic (WAS) profles were collected, crossing the Tyrrhenianbasin from side to side. the data were acquired with the Spanish R/V Sarmiento de Gamboain coordination with the Italian R/V Urania. The WAS data were also recorded by several landstations installed in Corsica and Sardinia (Fig. 1). The CHIANTI survey was carried out bythe R/V Sarmiento de Gamboa and two long Wide-Angle Seismic profles, CHIANTI-WAS 2and CHIANTI WAS 4 (Fig. 1), were collected. CHIANTI-WAS 2 is WNW-ESE trending andcrosses the deepest part of the Tyrrhenian Basin, from the Vavilov Basin to the Marsili Basin.The CHIANTI - WAS 4 is oriented almost N-S and crosses the whole Vavilov Basin, from theCampanian margin till the Sicilian margin.

The back-arc tyrrhenian basin opening history, new insights from a recent geophysical data acquisition

N Zitellini;MF Loreto;M Ligi;R de Franco
2017

Abstract

In 2010 and 2015 two geophysical surveys were carried out in the Tyrrhenian basin withinthe framework of a Spanish-German-Italian projects MEDOC and the CHIANTI, respectively.During the MEDoC survey a total of 17 Multichannel seismic (MCS) lines for a total length of2.808 km and 5 long Wide-Angle Seismic (WAS) profles were collected, crossing the Tyrrhenianbasin from side to side. the data were acquired with the Spanish R/V Sarmiento de Gamboain coordination with the Italian R/V Urania. The WAS data were also recorded by several landstations installed in Corsica and Sardinia (Fig. 1). The CHIANTI survey was carried out bythe R/V Sarmiento de Gamboa and two long Wide-Angle Seismic profles, CHIANTI-WAS 2and CHIANTI WAS 4 (Fig. 1), were collected. CHIANTI-WAS 2 is WNW-ESE trending andcrosses the deepest part of the Tyrrhenian Basin, from the Vavilov Basin to the Marsili Basin.The CHIANTI - WAS 4 is oriented almost N-S and crosses the whole Vavilov Basin, from theCampanian margin till the Sicilian margin.
2017
Istituto per la Dinamica dei Processi Ambientali - IDPA - Sede Venezia
Istituto di Scienze Marine - ISMAR
978-88-940442-8-7
Crustal structures Tyrrenian Basin
Crustal Geophysics
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.14243/341839
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