Ridge segmentation and the magnetic structure of the Southwest Indian Ridge (at 50°30′E, 55°30′E and 66°20′E): Implications for magmatic processes at ultraslow-spreading centers
Author:
Affiliation:
1. Institut de Physique du Globe de Strasbourg, CNRS-ULP; 5 rue René Descartes,; 67084; Strasbourg Cedex; France
2. Institut de Physique du Globe de Paris, CNRS-UPMC; 4 Place Jussieu,; 75252; Paris Cedex 05; France
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Reference52 articles.
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3. How thick is the magmatic crust at slow spreading oceanic ridges;Cannat;J. Geophys. Res.,1996
4. Gabbroic rocks trapped in the upper mantle at the Mid-Atlantic Ridge;Cannat;Proc. Ocean Drill. Program Sci. Results,1997
5. Formation of the axial relief at the very slow spreading Southwest Indian Ridge (49° to 69°E);Cannat;J. Geophys. Res.,1999
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