• A. S. Bookin
  • V. A. Drits
  • I. V. Rozdestvenskaya
  • T. F. Semenova
  • S. I. Tsipursky

The positions of hydroxyl protons in 2:1 layers of chlorites and micas are mainly determined by electrostatics. For the hydroxyls of dickite, amesite and the brucite sheets of chlorite, systematically different results are given by the two methods. Causes and implications of these results are discussed.-D.F.B.

Original languageEnglish
Pages (from-to)409-414
Number of pages6
JournalClays & Clay Minerals
Volume30
Issue number6
DOIs
StatePublished - 1 Jan 1982

    Scopus subject areas

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

ID: 50027343