Polytypism of Trioctahedral 1:1 Layer Silicates

@article{Bailey1969PolytypismOT,
  title={Polytypism of Trioctahedral 1:1 Layer Silicates},
  author={Steven W. D. Bailey},
  journal={Clays and Clay Minerals},
  year={1969},
  volume={17},
  pages={355-371}
}
Polytypism in trioctahedral 1 : 1 phyllosilicates results from two variable features in the structure. (1) The octabedral cations may occupy the same set of three positions throughout or may alternate regularly between two different sets of positions in successive layers. (2) Hydrogen bonding between adjacent oxygen and hydroxyl surfaces of successive layers can be obtained by three different relative positions of layers: (a) direct superposition of layers, (b) shift of the second layer by a/3… CONTINUE READING

Citations

Publications citing this paper.
SHOWING 1-10 OF 29 CITATIONS

The crystal structure of lizardite 1 T : hydrogen bon { s and polytypism

Mencelro, MBrtrNr, C. S. Geologia Strutturale
  • 2007
VIEW 5 EXCERPTS
CITES BACKGROUND
HIGHLY INFLUENCED