Structural and compositional variations of basic Cu(II) chlorides in the herbertsmithite and gillardite structure field

Matthew J. Sciberras, Peter Leverett, Peter A. Williams, Jochen Schlüter, Thomas Malcherek, Mark D. Welch, Peter J. Downes, David E. Hibbs, Anthony R. Kampf

Research output: Contribution to journalArticlepeer-review

2 Citations (Scopus)

Abstract

Natural samples of the substituted basic Cu(II) chloride series, Cu4-xM2+ x(OH)6Cl2 (M= Zn, Ni, or Mg) were investigated by single-crystal X-ray diffraction in order to elucidate compositional boundaries associated with paratacamite and its congeners. The compositional ranges examined are Cu3.65Zn0.35(OH)6Cl2" Cu3.36Zn0.64(OH)6Cl2 and Cu3.61Ni0.39(OH)6Cl2" Cu3.13Ni0.87(OH)6Cl2, along with a single Mg-bearing phase. The majority of samples studied have trigonal symmetry (Rʒ̅m) analogous to that of herbertsmithite (Zn) and gillardite (Ni), with a ≈ 6.8, c ≈ 14.0 Å. Crystallographic variations for these samples caused by composition are compared with both published and new data for the Rʒ̅m sub-cell of paratacamite, paratacamite-(Mg) and paratacamite-(Ni). The observed trends suggest that the composition of end-members associated with the paratacamite congeners depend upon the nature of the substituting cation.
Original languageEnglish
Pages (from-to)123-134
Number of pages20
JournalMineralogical Magazine
Volume81
Issue number1
DOIs
Publication statusPublished - 2017

Keywords

  • chlorides
  • crystals
  • gillardite
  • herbertsmithite
  • paratacamite

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