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The in situ formation and development of some kaolinite macrocrystals

Published online by Cambridge University Press:  14 March 2018

L. R. Moore
L. R. Moore*
Affiliation:
Department of Geology, University of Sheffield
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Abstract

Tonsteins, which are kaolinite-rich rocks with an amorphous groundmass containing much organic material, occur widely in European Coal Measure deposits. The nature of these rocks and their peculiar fabric is considered in detail and evidence is adduced which suggests that they were derived from soils and that the original organic components (micro-organisms and fungi) played a significant part in the formation of the kaolinite macrocrystals.

Type
Research Article
Information
Clay Minerals Bulletin , Volume 5 , Issue 31 , July 1964 , pp. 338 - 352
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1964

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