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Ba-Bearing Clinoptilolite from ODP Leg 127, Site 795, Japan Sea
Published online by Cambridge University Press: 28 February 2024
Abstract
Ba-bearing clinoptilolite (with >2 wt. % BaO) occurs in Neogene marine siliceous sediments from ODP Leg 127 Site 795 in the Japan Sea. Ba-bearing clinoptilolite is formed by reaction of volcanic glass and Ba-rich pore water during burial diagenesis.
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- Copyright © 1994, Clay Minerals Society
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