Abstract
The basalts are strongly LREE-depleted oceanic tholeiites. They resemble deep-ocean-floor basalts and are clearly different from continental tholeiites (flood basalts).-K.A.R.
Cite
CITATION STYLE
APA
Joron, J. L., Bougault, H., Maury, R. C., Bohn, M., & Desprairies, A. (1984). Strongly depleted tholeiites from the Rockall Plateau margin, North Atlantic: geochemistry and mineralogy. Initial Reports of the D.S.D.P., 81, 783–794. https://doi.org/10.2973/dsdp.proc.81.131.1984
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