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Major- and trace-element geochemistry of basalts from Ojin, Nintoku, and Suiko seamounts of the Emperor seamount chain: DSDP- IPOD Leg 55.

Initial Reports of the D.S.D.P. (1980) 55 599-605
DOI: 10.2973/dsdp.proc.55.124.1980
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Abstract

The alkali and tholeiitic basalts are similar in their major- and LIL trace-element chemistry to the alkali and tholeiitic basalts of Hawaii. Olivine fractionation seems to explain intrasite major-element compositional variations. Apparently the seamount basalts and the Hawaiian Island basalts do not come from a single hot-spot source. -K.A.R.English

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APA

Bence, A. E., Taylor, S. R., & Fisk, M. R. (1980). Major- and trace-element geochemistry of basalts from Ojin, Nintoku, and Suiko seamounts of the Emperor seamount chain: DSDP- IPOD Leg 55. Initial Reports of the D.S.D.P., 55, 599–605. https://doi.org/10.2973/dsdp.proc.55.124.1980

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