• journal_title：American Mineralogist
• Contributor：Marcus J. Origlieri ; Hexiong Yang ; Robert T. Downs ; Esther S. Posner ; Kenneth J. Domanik ; William W. Pinch
• Publisher：Mineralogical Society of America
• Date：2012-
• Format：text/html
• Language：en
• Identifier：10.2138/am.2012.4269
• journal_abbrev：American Mineralogist
• issn：0003-004X
• volume：97
• issue：10
• firstpage：1812
• section：Letters

Bartelkeite from Tsumeb, Namibia, was originally described by Keller et al. (1981) with the chemical formula PbFeGe₃O₈. By means of electron microprobe analysis, single-crystal X-ray diffraction, and Raman spectroscopy, we examined this mineral from the type locality. Our results show that bartelkeite is monoclinic with space group P2₁/m, unit-cell parameters a = 5.8279(2), b = 13.6150(4), c = 6.3097(2) Å, β = 127.314(2)°, and a revised ideal chemical formula PbFeGe^VIGe₂^IVO₇(OH)₂·H₂O (Z = 2). Most remarkably, bartelkeite is isostructural with the high-pressure P2₁/m phase of lawsonite, CaAl₂Si₂O₇(OH)·H₂O, which is only stable above 8.6 GPa and a potential host for H₂O in subducting slabs. Its structure consists of single chains of edge-sharing FeO₆ and Ge1O₆ octahedra parallel to the c-axis, cross-linked by Ge2₂O₇ tetrahedral dimers. The average <Ge-O> bond lengths for the GeO₆ and GeO₄ polyhedra are 1.889 and 1.744 Å, respectively. The Pb atoms and H₂O groups occupy large cavities within the framework. The hydrogen bonding scheme in bartelkeite is similar to that in lawsonite. Bartelkeite represents the first known mineral containing both 4- and 6-coordinated Ge atoms and may serve as an excellent analog for further exploration of the temperature-pressure-composition space of lawsonite.