Magmatic cycles and formation of the upper oceanic crust at spreading centers: Geochemical study of a continuous extrusive section in the Oman ophiolite

Author:

Einaudi F.,Godard M.1,Pezard P.1,Cochemé J.-J.2,Coulon C.2,Brewer T.3,Harvey P.3

Affiliation:

1. Laboratoire de Tectonophysique, ISTEEM, CNRS UMR5568; Université de Montpellier II; 34095; Montpellier, Cedex 5; France

2. Laboratoire de Pétrologie Magmatique; Université d'Aix Marseille, Faculté des Sciences de St Jérôme; 13397; Marseille Cedex 20; France

3. Department of Geology; University of Leicester; University Rd.,; Leicester; LE1 7RH; United Kingdom

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference83 articles.

1. Basement lithostratigraphy, DSDP Hole 504B, Leg 83;Adamson;Init. Rep. Deep Sea Drill. Proj.,1985

2. The interrelationship between magmatic and ore-forming hydrothermal processes in the Oman ophiolite;Alabaster;Econ. Geol.,1985

3. The volcanic stratigraphy and petrogenesis of the Oman ophiolite complex;Alabaster;Contrib. Mineral. Petrol.,1982

4. The ophiolite-radiolarite belt of the north Oman Mountains;Alleman;Eclogae Geol. Helv.,1972

5. Hydrothermal alteration of a section of upper oceanic crust in the eastern equatorial Pacific: A synthesis of results from Site 504 (DSDP Legs 69, 70, and 83, and ODP Legs 111, 137, 140, and 148);Alt;Proc. Ocean Drill. Program, Sci. Results,1996

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