Author:
Smithson Frank,Brown George
Abstract
AbstractThe clay mineral, dickite, is a common rock-forming mineral of many Carboniferous sandstones in North Wales and Northern England and of Middle Jurassic sandstones over much of North-East Yorkshire. It occurs as well-shaped authigenic crystals associated with highly altered mineral assemblages, including partly dissolved feldspar which is one of the probable sources of the alumina and silica.
Publisher
Cambridge University Press (CUP)
Cited by
3 articles.
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