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Dataset.

MEDOC Cruise, RV Sarmiento de Gamboa

Digital.CSIC. Repositorio Institucional del CSIC
oai:digital.csic.es:10261/232010
Digital.CSIC. Repositorio Institucional del CSIC
  • Ranero, César R.
  • CSIC - Unidad de Tecnología Marina (UTM)
MEDOC Cruise (29SG20100407) carried out on the Research Vessel Sarmiento de Gamboa in 2010, The Western Mediterranean basin: a natural laboratory of the processes of formation of continental margins extension. During the cruise collected 16 Multichannel Seismic Reflection (MCS) profiles using a 3.75 km-long streamer and a 3000 c.i. G-II gun array. Each transect provides the tectonic structure, the geometry of sedimentary deposits, and P-wave seismic velocity distribution. This information allows to interpret the mechanisms of deformation, infer the importance and potential role of magmatism in the rifting process, and estimate the region of mantle exhumation, currently inferred from one drill site. The analysis of the data provides insight in the process of formation of asymmetry structure conjugated margins
 
DOI: http://hdl.handle.net/10261/232010
Digital.CSIC. Repositorio Institucional del CSIC
oai:digital.csic.es:10261/232010

HANDLE: http://hdl.handle.net/10261/232010
Digital.CSIC. Repositorio Institucional del CSIC
oai:digital.csic.es:10261/232010
 
Ver en: http://hdl.handle.net/10261/232010
Digital.CSIC. Repositorio Institucional del CSIC
oai:digital.csic.es:10261/232010
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Digital.CSIC. Repositorio Institucional del CSIC
oai:digital.csic.es:10261/232010
Dataset. 2010

MEDOC CRUISE, RV SARMIENTO DE GAMBOA

Digital.CSIC. Repositorio Institucional del CSIC
  • Ranero, César R.
  • CSIC - Unidad de Tecnología Marina (UTM)
MEDOC Cruise (29SG20100407) carried out on the Research Vessel Sarmiento de Gamboa in 2010, The Western Mediterranean basin: a natural laboratory of the processes of formation of continental margins extension. During the cruise collected 16 Multichannel Seismic Reflection (MCS) profiles using a 3.75 km-long streamer and a 3000 c.i. G-II gun array. Each transect provides the tectonic structure, the geometry of sedimentary deposits, and P-wave seismic velocity distribution. This information allows to interpret the mechanisms of deformation, infer the importance and potential role of magmatism in the rifting process, and estimate the region of mantle exhumation, currently inferred from one drill site. The analysis of the data provides insight in the process of formation of asymmetry structure conjugated margins

HANDLE: http://hdl.handle.net/10261/232010


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