Abstract
Apparently the ferrobasalts form in isolated magma chambers, which prevents them from mixing with primitive olivine tholeiite supplied to the East Pacific Rise magma chamber. (Preceding abstracts) -K.A.R.
Cite
CITATION STYLE
APA
Natland, J. H. (1980). Effect of axial magma chambers beneath spreading centers on the compositions of basaltic rocks. Initial Reports of the D.S.D.P., 54, 833–850. https://doi.org/10.2973/dsdp.proc.54.138.1980
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