Abstract
The Mossbauer analyses were performed on saponite samples which were kept in an N-purged container until analysis. The study shows that Fe3+ remained in octahedral coordination and no changes occurred in the physical appearance of the sample.-K.A.R.
Cite
CITATION STYLE
APA
Andrews, A. J., Dollase, W. A., & Fleet, M. E. (1983). A Mossbauer study of saponite in layer 2 basalt, Deep Sea Drilling Project Leg 69. Initial Reports of the D.S.D.P., 69, 585–588. https://doi.org/10.2973/dsdp.proc.69.131.1983
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