Jump to: Page Content, Section Navigation, Site Navigation, Site Search, Account Information, or Site Tools.
|
|
Articles
Red Sea Floor Origin: Rare-Earth Evidence
1 Graduate School of Oceanography, University of Rhode Island, Kingston 02881
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.
THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
|
Science. ISSN 0036-8075 (print), 1095-9203 (online)