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={W. Noll},
  journal={Zeitschrift f{\"u}r Kristallographie, Mineralogie und Petrographie},
  year={1936},
  volume={48},
  pages={210-247}
}
  • W. Noll
  • Published 1936
  • Geology
  • Zeitschrift für Kristallographie, Mineralogie und Petrographie
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References

SHOWING 1-10 OF 16 REFERENCES
THE KAOLIN MINERALS1
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,Expand
THE MINERALS OF BENTONITE AND RELATED CLAYS AND THEIR PHYSICAL PROPERTIES1
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 rockExpand
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