Abstract

High resolution imaging by TEM has revealed a mechanism for the weathering of intermediate microcline in a humid, temperate climate. Dissolution of the feldspar begins at the boundary of twinned and untwinned domains and produces circular holes which enlarge to form negative crystals. Amorphous, ring-shaped structures develop, about 25 Angstrom in diameter, within the larger holes. These rings, in turn, crystallize to an arcuate phase and then to crinkled sheets of illite or dehydrated montmorillonite. -from Authors

Original languageEnglish (US)
Pages (from-to)173-178
Number of pages6
JournalClays and Clay Minerals
Volume28
Issue number3
DOIs
StatePublished - Jan 1 1980

ASJC Scopus subject areas

  • Water Science and Technology
  • Soil Science
  • Geochemistry and Petrology
  • Earth and Planetary Sciences (miscellaneous)

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