Author:
Farmer V. C.,Fraser A. R.,Russell J. D.,Yoshinaga N.
Abstract
AbstractImogolite structures in allophanic clays can be recognized and semi-quantitatively estimated by an absorption band at 348 cm−1. Allowance can be made for interference by aluminous dioctahedral layer silicates present in small amounts.
Subject
Geochemistry and Petrology
Cited by
67 articles.
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