Thin-skinned and low-angle extensional faulting - A Structural model for the Gulf of Lion margin

A. Benedicto; P. Labaume; M. Serrane; M. Seguret; C. Truffert; IBS-Gulfof Lion Working Group

doi:10.3997/2214-4609.201410286

f Thin-skinned and low-angle extensional faulting - A Structural model for the Gulf of Lion margin
By A. Benedicto, P. Labaume, M. Serrane, M. Seguret, C. Truffert and IBS-Gulfof Lion Working Group
Publisher: European Association of Geoscientists & Engineers
Source: Conference Proceedings, 56th EAEG Meeting, Jun 1994, cp-47-00531
ISBN: 978-90-73781-05-4
DOI: https://doi.org/10.3997/2214-4609.201410286

Abstract

The Gulf of Lion area corresponds to the NW rifted margin of the NW-Mediterranean basin. Oceanic accretion occurred during the Burdigalian, following an Oligocene-Aquitanian rifting episode.

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1994-06-10

2024-04-16

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Abstract

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The natural combination of full and image‐based waveform inversion

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Characterizing the effect of elastic interactions on the effective elastic properties of porous, cracked rocks

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Laboratory measurements of guided‐wave propagation within a fluid‐saturated fracture