Seismic Crustal Features of Adria Plate Offshore

A. Del Ben; A. Battigelli; R. Geletti; M. Pipan; I. Finetti

doi:10.3997/2214-4609.201408430

f Seismic Crustal Features of Adria Plate Offshore
By A. Del Ben, A. Battigelli, R. Geletti, M. Pipan and I. Finetti
Publisher: European Association of Geoscientists & Engineers
Source: Conference Proceedings, 60th EAGE Conference and Exhibition, Jun 1998, cp-110-00331
ISBN: 978-90-73781-09-2
DOI: https://doi.org/10.3997/2214-4609.201408430

Abstract

Tha Adria Plate is generally considered a wide carbonate platform of principalley Mesozoic age (but started in Late Paleozoic age) covering an original African promontory. From a Triassic rifting phase, this promontory began its separation from megaplate and its northward migration and anticlockwise rotation (Finetti, 84).

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1998-06-08

2024-04-20

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f Seismic Crustal Features of Adria Plate Offshore

Abstract

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