Using XRD, XRF, AA and SEM, two diagenetic alterations are inferred. Low-T alteration formed smectite and zeolites (phillipsite and clinoptilolite). The second occurs in sediments overlying the basalts and the altered basalts themselves, and this hydrothermal phase produced palygorskite. -K.A.R.
CITATION STYLE
Desprairies, A. (1982). Authigenic minerals in volcanogenic sediments cored during Deep Sea Drilling Project Leg 60. Initial Reports of the D.S.D.P., 60, 455–466. https://doi.org/10.2973/dsdp.proc.60.120.1982
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