Peterandresenite | |
Category: | Oxide, Hexaniobate |
Formula: | Mn4Nb6O19•14H2O |
Imasymbol: | Pan[1] |
System: | Monoclinic |
Class: | Prismatic (2/m) (same H-M symbol) |
Symmetry: | C2/m |
Unit Cell: | a = 15.33, b = 9.41, c = 11.28 [Å], β = 118.65° (approximated); Z = 2 |
Color: | Orange |
Habit: | crystals (equidimensional) |
Cleavage: | None |
Fracture: | Uneven |
Tenacity: | Brittle |
Mohs: | 2-2.5 |
Luster: | Vitreous or resinous |
Streak: | Pale orange |
Density: | 3.05 (calc.), 3.10 (meas.) [g/cm<sup>3</sup>] |
Diaphaneity: | Transparent or translucent |
References: | [2] |
Peterandresenite is a very rare mineral,[3] the first known natural hexaniobate. Its chemical formula is Mn4Nb6O19•14H2O. Its structure contains a special type of octahedron: Lindqvist ion. Peterandresenite was found in a pegmatite of the Larvik complex in Norway.[4] It is somewhat similar to other unique niobium minerals, aspedamite and menezesite.[5] [6]
Peterandresenite was discovered in AS Granit quarry, Tvedalen, Larvik, Vestfold, Norway.