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Formula:
[K(H2O)]Mn2(Ti2Fe3+)(PO4)4O2(H2O)10.4H2O
Phosphate, paulkerrite group,
manganese- and titanium- bearing
mineral
Crystal System: Orthorhombic
Specific gravity: 2.40 calculated
Colour: Pale yellow
Environments
Hochleitnerite is a new mineral, approved in 2023 and to date (November 2024) reported only from the type locality.
Localities
At the type locality, the Hagendorf South Pegmatite, Hagendorf, Waidhaus, Neustadt an der Waldnaab District, Upper
Palatinate, Bavaria, Germany, hochleitnerite crystals occur on altered
zwieselite. Minerals closely associated with hochleitnerite and
zwieselite are rockbridgeite,
fluorapatite, columbite and
sub-micrometre rods of uranophane. Other associated minerals are
quartz and a jahnsite group
mineral.
Titanium-bearing minerals are very rare at Hagendorf Süd, with only
biotite, ilmenite and a variety of the
pyrochlore group recorded in Mindat. The most likely source of the
titanium in hochleitnerite is the altered
zwieselite matrix that it is in contact with. The presence of
hochleitnerite crystals lining vugs formed by leaching of zwieselite
suggests that hochleitnerite formed from zwieselite by
dissolution–reprecipitation, and the presence of considerable H2O in its formula indicates that this occurred
at a relatively low temperature
(EJM 35.4.635-643).
Hochleitnerite from the Hagendorf South
Pegmatite - Image
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