Abstract
The oxygen isotope compositions of whole-rock basalt samples suggest only limited amounts of low-T sea-water-basalt interaction. Plagioclase-magnetite fractionation values imply crystallization under closed-system conditions.-K.A.R.
Cite
CITATION STYLE
APA
Hoernes, S., & Friedrichsen, H. (1983). Oxygen isotopic composition of basalts from Leg 65, Deep Sea Drilling Project. Initial Reports of the D.S.D.P., 65, 661–665. https://doi.org/10.2973/dsdp.proc.65.132.1983
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