Abstract
The green clays were analysed by XRD, IR, electron diffraction and chemical analysis, which show that mixed-layer celadonite and nontronite dominate. Computer factor analysis indicates two stages of hydrothermal activity (early and late stages of the Late Pleistocene). The Mn compounds and their associates were formed during the early stage at low T.-K.A.R.
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CITATION STYLE
APA
Varentsov, I. M., Sakharov, B. A., Drits, V. A., Tsipursky, S. I., Choporov, D. Y., & Aleksandrova, V. A. (1983). Hydrothermal deposits of the Galapagos rift zone, Leg 70: mineralogy and geochemistry of major components. Initial Reports of the D.S.D.P., 70, 235–268. https://doi.org/10.2973/dsdp.proc.70.111.1983
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