title: Red sea floor origin: rare-Earth evidence.
abstract: Abundance patterns of rare earths of submarine tholeiitic basalts from the axial trough of the Red Sea resemble those of basalts from mid-ocean ridges but are distinct from shield or plateau basalts of tholeiitic composition. These results imply that à similar magmatic process, related to spreading of sea floors, operates beneath the axial trough of the Red Sea and the crest of mid-ocean ridges.
authors.forename: J G
authors.initials: JG
authors.lastname: Schilling