Über die Bildungsbedingungen von Kaolin, Montmorillonit, Sericit, Pyrophyllit und Analcim

@article{Noll1936berDB,
  title={{\"U}ber die Bildungsbedingungen von Kaolin, Montmorillonit, Sericit, Pyrophyllit und Analcim},
  author={Walter Noll},
  journal={Zeitschrift f{\"u}r Kristallographie, Mineralogie und Petrographie},
  year={1936},
  volume={48},
  pages={210-247}
}
  • W. Noll
  • Published 1 July 1936
  • Geology
  • Zeitschrift für Kristallographie, Mineralogie und Petrographie

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A report of an investigation of the clay minerals, nacrite, diekite, and kaolinite is presented in which the methods of study are explained. The optical and physical properties, chemical composition,

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Bentonite is a very widely distributed clay material that is the result of the devitrification and chemical alteration of glassy volcanic ash or tuff. Bentonite should be used as the name of a rock

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This paper embodies the results of a study of the regional and local alterations which have affected a series of volcanic rocks lying around the borders of the head of Conception Bay, on the Avalon