| Classification |
|---|
|
| Species: | 'Apatite' (not an IMA approved species) |
| Formula: | Ca5(PO4)3(Cl/F/OH) |
| Confirmation |
|---|
|
| Validity: | Believed Valid |
| Data |
|---|
|
| Mineral Data: | Click here to view Apatite data |
| Locality Data: | Click here to view Größenberg, Eppenstein, Weißkirchen in Steiermark, Murtal District, Styria, Austria |
| Data Identifiers |
|---|
|
| Mindat Occurrence Record ID: | 1621768 |
| Long-form Identifier: | 1:3:1621768:3 |
| GUID (UUID V4): | 89764a55-0c3f-43a3-8d79-2bb11de1c73b |
| Nearest other occurrences of Apatite |
|---|
|
|
| 5.2km (3.3 miles) | ⓘLeucophyllite mine, Kothgraben (Kotgraben), Kleinfeistritz, Weißkirchen in Steiermark, Murtal District, Styria, Austria |
| 18.6km (11.5 miles) | ⓘA2 Highway tunnel, Übelskogel, Bad Sankt Leonhard im Lavanttal, Wolfsberg District, Carinthia, Austria |
| 19.5km (12.1 miles) | ⓘPuchbach (Grabenmühle), Maria Lankowitz, Voitsberg District, Styria, Austria |
| 19.9km (12.4 miles) | ⓘHematite Mine, Waldenstein, Wolfsberg, Wolfsberg District, Carinthia, Austria |
| 23.1km (14.3 miles) | ⓘKlementkogel, Hirschegg-Pack, Voitsberg District, Styria, Austria |
| 26.4km (16.4 miles) | ⓘMagnetite prospect, Kleinwöllmiß, Sankt Martin am Wöllmißberg, Voitsberg District, Styria, Austria |
| 26.9km (16.7 miles) | ⓘEbenlecker farm (Ebenlöcker farm; Ebenlecker quarry), Herzogberg, Modriach, Edelschrott, Voitsberg District, Styria, Austria |
| 27.3km (16.9 miles) | ⓘKamperkogel, Frantschach-Sankt Gertraud, Wolfsberg District, Carinthia, Austria |
| 28.2km (17.5 miles) | ⓘGroßer Ringkogel, Gaal, Murtal District, Styria, Austria |
| 28.6km (17.8 miles) | ⓘStoffhütte pegmatite, Deutschlandsberg, Deutschlandsberg District, Styria, Austria |
| References |
|---|
|
|
| Reference Search (possible matching items) |
|---|
 | | Journal (article/letter/editorial) | | only rich in fluid inclusions, quartz also contains traces of hydrogen which are incorporated in its crystal...crystal structure in form of OH groups. OH contents in dry mineral systems are of geologic interest as...perpendicular to the c-axis of quartz from Alpine veins in the Penninic Zone, the Greywacke Zone, and the Central...B-OH band. In type B the Li-OH band shows an intensity even to that of the Al-OH band. In type C Al-OH...be observed. In type D only the Al-OH band is present. Spectra type A is dominating in quartz with relatively |
|
