Bartelkeite | |
Category: | Germanate mineral |
Formula: | PbFeGe(Ge2O7)(OH)2•H2O |
Imasymbol: | Btk[1] |
Strunz: | 9.J0.10 (10 ed) 4/C.08-60 (8 ed) |
Dana: | 7.6.2.1 |
System: | Monoclinic |
Class: | Spheroidal (2) or prismatic (2/m) |
Symmetry: | P21 or P21/m |
Unit Cell: | a = 5.83, b = 13.62, c = 6.31 [Å], β = 127.31° (approximated); Z = 2 |
Color: | Colorless, white, very pale greenish |
Habit: | tabular; acicular |
Cleavage: | , distinct |
Mohs: | 4 |
Luster: | Subadamantine |
Streak: | White |
Diaphaneity: | Transparent |
Density: | 4.97 |
Opticalprop: | Biaxal (-) |
Refractive: | nα=1.89, nβ=1.91, nγ=1.91 (approximated) |
2V: | ca. 35o (measured) |
References: | [2] |
Bartelkeite is an exceptionally rare mineral, one of scarce natural germanium compounds.[3] The formula was originally assumed to be PbFeGe3O8,[4] bartelkeite was later shown to be isostructural with a high-pressure form of the mineral lawsonite. Thus, its correct formula is PbFeGe(Ge2O7)(OH)2•H2O.[5] Bartelkeite and mathewrogersite are minerals with essential (dominant) lead, iron and germanium.[6] Both come from Tsumeb, Namibia - a world's "capital" of germanium minerals.[7]
Bartelkeite was detected in voids of germanium ore occurring within dolomites. The mineral associates with galena, germanite, reniérite, and tennantite.
Bartelkeite is the first analyzed mineral containing both tetrahedrally- and octahedrally-coordinated germanium. It is isostructural with high-pressure form of the silicate lawsonite. In the structure there are: