Abstract
The basalt samples are typical light-REE-depleted normal oceanic crust. This implies that large, long-lived magma chambers do not exist at the axis of the Rise.-K.A.R.
Cite
CITATION STYLE
APA
Cambon, P., Bougault, H., Joron, J. L., & Treuil, M. (1983). Basalts from the East Pacific Rise: an example of typical oceanic crust depleted in hygromagmaphile elements. Initial Reports of the D.S.D.P., 65, 623–633. https://doi.org/10.2973/dsdp.proc.65.129.1983
Register to see more suggestions
Mendeley helps you to discover research relevant for your work.
Already have an account? Sign in
Sign up for free