Crustal structure of the continent-ocean transition off the Côte d'Ivoire-Ghana transform margin: implications for thermal exchanges across the palaeotransform boundary-Reference-Cited by-同舟云学术

Crustal structure of the continent-ocean transition off the Côte d'Ivoire-Ghana transform margin: implications for thermal exchanges across the palaeotransform boundary

Published:2000-12 Issue:3 Volume:143 Page:662-678
ISSN:0956-540X
Container-title:Geophysical Journal International
language:en
Short-container-title:

Author:

Sage F.,Basile CH.,Mascle J.,Pontoise B.,Whitmarsh R. B.

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

Link

http://academic.oup.com/gji/article-pdf/143/3/662/2133012/143-3-662.pdf

Reference75 articles.

1. The relationship between seismic velocity and density in the continental crust-a useful constraint?;Barton;Geophys. J. R. astr. Soc.,1986

2. The Ivory Coast-Ghana transform margin: a marginal ridge structure deduced from seismic data;Basile;Tectonophysics,1993

3. Enregistrement structural du coulissage Afrique/Brésil au sein des sédiments crétacés de la marge transformante de Côte d'Ivoire-Ghana;Benkhelil;C. R. Acad. Sci. Paris,1996

4. Submersible observations of Cretaceous deformations along the Côte d'Ivoire-Ghana transform margin;Benkhelil;Geo-Mar. Lett.,1997

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