1. Agrinier, P., Mével, C. and Girardeau, J., 1988. Hydrothermal alteration of the peridotites cored at the ocean/continent boundary of the Iberian margin: petrologic and stable isotope evidence. In: G. Boillot, E.L. Winterer et al. (Editors), Proc. of the ODP, Scientific Results, 103: 225–234.
2. Aumento, F. and Loubat, H., 1971. The Mid-Atlantic Ridge near 45°N. XVI. Serpentinized ultramafic intrusions. Canad. Journ. Earth Sci., 8: 631–663.
3. Benn, K., Nicolas, A. and Reuber, I., 1988. Mantle-crust transition zone and origin of wehrlitic magmas: evidence from the Oman ophiolite. Tectonophysics, 151: 75–85.
4. Bergès, J.P.,1989. Modélisation gravimétrique de la ride Médio-Atlantique: mur Ouest et Snake Pit à la latitude 23°20′N, Rapport DEA, Université de Paris VI.
5. Bloomer, S.H., Natland, J.H. and Fisher, R.L., 1989. Mineral relationships in gabbroic rocks from fracture zones of Indian Ocean ridges: evidence for extensive fractionation, parental diversity, and boundary-layer recrystallization. In: A.D. Saunders and M.J. Norry (Editors), Magmatism in the Ocean Basins. Geol. Soc. London Spec. Publ., 42: 107–124.