Geochemical Constrains on MORB Composition and Magma Sources at East Pacific Rise Between 1°S and 2°S
Author:
Publisher
Springer Science and Business Media LLC
Subject
Ocean Engineering,Oceanography
Link
http://link.springer.com/article/10.1007/s11802-018-3223-5/fulltext.html
Reference24 articles.
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2. Eason, D., and Sinton, J., 2006. Origin of high-Al N-MORB by fractional crystallization in the upper mantle beneath the Galápagos Spreading Center. Earth and Planetary Science Letters, 252: 423–436.
3. Farley, K. A., Basu, A. R., and Craig, H., 1993. He, Sr and Nd isotopic variations in lavas from the Juan Fernandez Archipelago, SE Pacific. Contributions to Mineralogy and Petrology, 115: 75–87.
4. Fornari, D. J., Perfit, M. R., Allan, J. F., Batiza, R., Haymon, R., Barone, A., Ryan, W. B. F., Smith, T., Simkin, T., and Luckman, M. A., 1988. Geochemical and structural studies of the Lamont seamounts: Seamounts as indicators of mantle process. Earth and Planetary Science Letters, 89: 63–83.
5. Frey, F. A., Walker, N., Stakes, D., Hart, S. R., and Nielson, R., 1993. Geochemical characteristics of basaltic glasses from the AMAR and FAMOUS axial valleys, Mid-Atlantic Ridge (36°–37°N): Petrogenetic implications. Earth and Planetary Science Letters, 115: 117–136.
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