| Locality type: | Quarry |
| Classification |
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| Species: | Magnesite |
| Formula: | MgCO3 |
| Confirmation |
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| Validity: | Believed Valid |
| Data |
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| Mineral Data: | Click here to view Magnesite data |
| Locality Data: | Click here to view Lower serpentinite quarry, Zwettler Leiten, Felling, Gföhl, Krems-Land District, Lower Austria, Austria |
| Data Identifiers |
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| Mindat Occurrence Record ID: | 1410511 |
| Long-form Identifier: | 1:3:1410511:7 |
| GUID (UUID V4): | 34bde08f-cb32-4f31-9059-9308b449d7e5 |
| Nearest other occurrences of Magnesite |
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| 4.4km (2.7 miles) | ⓘKlein-Heinrichschlag, Albrechtsberg an der Großen Krems, Krems-Land District, Lower Austria, Austria |
| 8.6km (5.3 miles) | ⓘDörrmühle (Hofmühle), Rastbach, Gföhl, Krems-Land District, Lower Austria, Austria |
| 11.6km (7.2 miles) | ⓘTrandorf, Mühldorf, Krems-Land District, Lower Austria, Austria |
| 11.6km (7.2 miles) | ⓘTurquoise ditch (Weinberg Forest), Amstall, Mühldorf, Krems-Land District, Lower Austria, Austria |
| 18.5km (11.5 miles) | ⓘMitterbachgraben, Gansbach, Dunkelsteinerwald, Melk District, Lower Austria, Austria |
| 22.7km (14.1 miles) | ⓘWanzenau, Gars am Kamp, Horn District, Lower Austria, Austria |
| 24.2km (15.0 miles) | ⓘSand pit, Rosenthal, Karlstetten, Sankt Pölten-Land District, Lower Austria, Austria |
| 38.5km (23.9 miles) | ⓘ"In der Gleisen" quarry (Yspertal; Ispertal; Unterfell), Sankt Oswald, Melk District, Lower Austria, Austria |
| 43.1km (26.8 miles) | ⓘGraphite quarry, Wollmersdorf (Zettlitz-Wollmersdorf), Drosendorf-Zissersdorf, Horn District, Lower Austria, Austria |
| 43.4km (27.0 miles) | ⓘSerpentinite quarry, Pingendorf, Drosendorf-Zissersdorf, Horn District, Lower Austria, Austria |
| References |
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| Reference Search (possible matching items) |
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 | | Journal (volume) | | Natans L. in Süd-Pohjanmaa . .. 5. VLADI MARMO, Serpentinite of Pahta-autsi, Finnish Lapland . . . . . ....Canada Geol. lnst., Melkweg I, Groningen, Neder· land Geophysical Laboratory, 2801 Upton St., N. W., Washington...occured at the high hydrothermal stage and at a lower temperature than the main sulphide ore of Orijärvi...displaced by slip page and rotation, because of the lower cohesionty between the fragments in the fractured...will probably find that the b-lineation is of a lower angle and more strongly developed. A promising way |  | | Journal (volume) | | Natans L. in Süd-Pohjanmaa . .. 5. VLADI MARMO, Serpentinite of Pahta-autsi, Finnish Lapland . . . . . ....Canada Geol. lnst., Melkweg I, Groningen, Neder· land Geophysical Laboratory, 2801 Upton St., N. W., Washington...occured at the high hydrothermal stage and at a lower temperature than the main sulphide ore of Orijärvi...displaced by slip page and rotation, because of the lower cohesionty between the fragments in the fractured...will probably find that the b-lineation is of a lower angle and more strongly developed. A promising way |  | Johnson, Scott E., Paterson, Scott R., Fletcher, John M., Girty, Gary H., Kimbrough, David L., Martín-Barajas, Arturo - Eds. (2003) Tectonic evolution of northwestern Mexico and the Southwestern USA. GSA Special Paper 374. Geological Society of America doi:10.1130/0-8137-2374-4 | Report (issue) | | batholith magmas were generated by melting of mafic lower-arc crust. Vill The following four papers present...denudation between 91 and 86 Ma and removal of lower crust and mantle lithosphere triggered erosional...of El Arco (28°N), upper-greenschist facies to lower-amphibolite facies quartzite and pelitic schist...forearc basin turbidites that range in age from lower Aptian (R. Sedlock, unpubl. data) to middle Eocene...event. The structurally intermediate unit is a serpentinite-matrix mélange that occupies fault zones up |
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