Author:
Justo A.,Maqueda C.,Pérez-Rodríguez J. L.,Lagaly G.
Abstract
AbstractA lamellar macroscopic Mg-vermiculite from Santa Olalla, Spain, which is accompanied by some talc and mica, shows a reversible expansion on glycolation due to the presence of layers with two different charges. The most probable origin of the vermiculite is by low-temperature hydrothermal transformation of phlogopite.
Subject
Geochemistry and Petrology
Cited by
7 articles.
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