Abstract
Carbonate isotope studies reveal that the associated basalts had an early, shallow-water phase, and a later deeper-water environment. -K.A.R.
Cite
CITATION STYLE
APA
McKenzie, J. (1980). Stable isotopic study of carbonate minerals from the basalt flows on Suiko seamount: DSDP Leg 55, hole 433C. Initial Reports of the D.S.D.P., 55, 653–657. https://doi.org/10.2973/dsdp.proc.55.127.1980
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