• journal_title：American Mineralogist
• Contributor：Ulf Hålenius ; Ferdinando Bosi
• Publisher：Mineralogical Society of America
• Date：2012-
• Format：text/html
• Language：en
• Identifier：10.2138/am.2012.4137
• journal_abbrev：American Mineralogist
• issn：0003-004X
• volume：97
• issue：10
• firstpage：1635
• section：Articles

A multi-analytical approach using electron microprobe analysis, X-ray structural refinement, and polarized single-crystal Fourier transform infrared spectroscopy was used to characterize short-range and long-range structures of a Pb²⁺-bearing, Mn³⁺-rich pargasite. Site populations, derived from the results of site-scattering refinement and stereochemical analysis, demonstrate that Pb²⁺ is strongly ordered at the A-site in the monoclinic C2/m amphibole structure. This finding is in agreement with the observed ordering of Pb²⁺ in the rare Pb²⁺-bearing P2/a amphibole joesmithite, but is in contrast to a Pb²⁺ preference for the M4 site suggested by some studies on element partitioning between C2/m amphiboles and melts. Mn³⁺ is strongly ordered at the M2 site in structure of the present amphibole. Contrasting results obtained for mean M2-O bond lengths and reported local Mn³⁺-O bond lengths as well as between bond-length distortion of the mean M2 polyhedron and the local Mn³⁺-centered M2O₆ octahedron in pargasite indicates that the structural relaxation of this polyhedron is complete or nearly so.