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Bulletin de la Societe Geologique de France; March 2008; v. 179; no. 2; p. 129-137; DOI: 10.2113/gssgfbull.179.2.129
© 2008 Societe Geologique de France
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Régime thermique de la marge nord-ouest du golfe du Mexique. Partie A: Champs de température et de pression

Laurent Husson1,2, Pierre Henry1 and Xavier Le Pichon1

1 Collège de France, Chaire de Géodynamique, Europôle de l’Arbois, 13545 Aix-en-Provence, France. henry{at}cdf.u-3mrs.fr (P. Henry); lepi-chon{at}cdf.u-3mrs.fr (X. Le Pichon)
2 Géosciences Rennes, UMR CNRS 6118, Université de Rennes 1, Campus de Beaulieu, 35042 Rennes cedex, France. laurent.husson{at}univ-rennes1.fr (L. Husson)

Le régime thermique du golfe du Mexique (GoM – Gulf of Mexico) est examiné à partir d’une base de 8 500 données de températures de fond de puit et de températures de réservoir. Notre analyse stochastique révèle une augmentation brutale systématique et régionale du gradient de température entre 2 500 et 4 000 m. L’analyse du régime de pres-sion montre une corrélation entre les champs de température et de pression.

Key Words: Golfe du Mexique • Géotherme • Pression




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