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 language | English |
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Pages (from-to) | 123-134 |
Number of pages | 20 |
Journal | Mineralogical Magazine |
Volume | 81 |
Issue number | 1 |
DOIs | |
Publication status | Published - 2017 |
Keywords
- chlorides
- crystals
- gillardite
- herbertsmithite
- paratacamite