Perturbative Theory of Mica Polytypism. Role of the M2 Layer in the Formation of Inhomogeneous Polytypes

Massimo Nespolo
  • Clays and Clay Minerals, January 2001, Clay Minerals Society
  • DOI: 10.1346/ccmn.2001.0490101

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http://dx.doi.org/10.1346/ccmn.2001.0490101

The following have contributed to this page: Distinguished Professor Massimo Nespolo