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Luis Somoza

Researcher at Instituto Geológico y Minero de España

Publications -  213
Citations -  7771

Luis Somoza is an academic researcher from Instituto Geológico y Minero de España. The author has contributed to research in topics: Continental shelf & Contourite. The author has an hindex of 49, co-authored 209 publications receiving 6989 citations. Previous affiliations of Luis Somoza include University of Salamanca & University of Santiago de Compostela.

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The quest for the Africa–Eurasia plate boundary west of the Strait of Gibraltar

TL;DR: In this article, a set of almost linear and sub-par dextral strike-slip faults, the SWIM1 Faults, that form a narrow band of deformation over a length of 600 km coincident with a small circle centred on the pole of rotation of Africa with respect to Eurasia, was mapped using a new swath bathymetry compilation available in the area offshore SW Portugal.
Journal ArticleDOI

The Betic orogen and the Iberian-African boundary in the Gulf of Cadiz: geological evolution (central North Atlantic)

TL;DR: In this paper, the evolution of the southern Iberian margin was more complex than in most North Atlantic margins since it entailed several phases of rifting, convergence and strike-slip motions.

The Quest for the Africa-Eurasia plate boundary West of the Strait of Gibraltar

TL;DR: In this article, a set of almost linear and sub-par dextral strike-slip faults, the SWIM1 Faults, that form a narrow band of deformation over a length of 600 km coincident with a small circle centred on the pole of rotation of Africa with respect to Eurasia, was mapped using a new swath bathymetry compilation available in the area offshore SW Portugal.
Journal ArticleDOI

Seabed morphology and hydrocarbon seepage in the Gulf of Cádiz mud volcano area: Acoustic imagery, multibeam and ultra-high resolution seismic data

Luis Somoza
- 30 Mar 2003 - 
TL;DR: In this paper, the Guadalquivir Diapiric Ridge (GDR) and Cadiz Diapirs (CDR) are longitudinally shaped diapirs which trend NE-SW and consist of lower-middle Miocene plastic marly clays.