Abstract
AbstractThe smectic clay from Sierra de Gata, Cabo de Gata region, Almería, Spain, is montmor-illonoidal like the smectic clay from Serrata de Nijar in the same region. These clays are formed by alteration of calco-alkaline volcanic rocks by marine and/or hydrothermal action.
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More From: Clays and clay minerals (National Conference on Clays and Clay Minerals)
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