| Locality type: | Quarry |
| Classification |
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| Species: | Cordierite |
| Formula: | (Mg,Fe)2Al3(AlSi5O18) |
| Confirmation |
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| Validity: | Believed Valid |
| Data |
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| Mineral Data: | Click here to view Cordierite data |
| Locality Data: | Click here to view Lower serpentinite quarry, Zwettler Leiten, Felling, Gföhl, Krems-Land District, Lower Austria, Austria |
| Photo Gallery | View Gallery (5 photos) |
| Data Identifiers |
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| Mindat Occurrence Record ID: | 654786 |
| Long-form Identifier: | 1:3:654786:8 |
| GUID (UUID V4): | c9ce9c87-04a8-42a2-8c2c-04b3be33c9cd |
| Nearest other occurrences of Cordierite |
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| 0.4km (0.2 miles) | ⓘZwettler Leiten, Felling, Gföhl, Krems-Land District, Lower Austria, Austria |
| 1.3km (0.8 miles) | ⓘHartenstein castle, Maigen, Weinzierl am Walde, Krems-Land District, Lower Austria, Austria |
| 2.2km (1.4 miles) | ⓘCordierite occurrence, Felling, Gföhl, Krems-Land District, Lower Austria, Austria |
| 3.4km (2.1 miles) | ⓘHohenstein, Gföhl, Krems-Land District, Lower Austria, Austria |
| 4.4km (2.7 miles) | ⓘKlein-Heinrichschlag, Albrechtsberg an der Großen Krems, Krems-Land District, Lower Austria, Austria |
| 18.7km (11.6 miles) | ⓘSchwaigbichl (Schwaigbichel), Hessendorf, Dunkelsteinerwald, Melk District, Lower Austria, Austria |
| 28.4km (17.6 miles) | ⓘGneiss quarry, Ebersdorf, Klein-Pöchlarn, Melk District, Lower Austria, Austria |
| 37.9km (23.6 miles) | ⓘHäuslern, Groß-Gerungs, Zwettl District, Lower Austria, Austria |
| 45.5km (28.3 miles) | ⓘHengl quarry, Eibenstein an der Thaya, Raabs an der Thaya, Waidhofen an der Thaya District, Lower Austria, Austria |
| 63.8km (39.6 miles) | ⓘMoserberg, Grünbach, Freistadt District, Upper Austria, Austria |
| References |
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Pristacz, H., Kolitsch, U., Löffler, E. & Knobloch, G. (2009): 1597) Cordierit, Dumortierit, Fluorapatit, Monazit, Rutil und Turmalin aus einem Pegmatit in einem Serpentinitsteinbruch bei der Zwettler Leiten, Felling, Waldviertel, Niederösterreich. Pp. 216-218 in: Niedermayr, G. et al. (2009): Neue Mineralfunde aus Österreich LVIII. Carinthia II, 199/119, 189-236. |
| Reference Search (possible matching items) |
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 | | Journal (article/letter/editorial) | | the top of the succession, whereas pyroxenites lower in the succession show varying degrees of interaction...fine-tomedium grained peridotites ascribed to the Lower Zone are equated with the pyroxenites, harzburgites...separated from each other by interlayers of serpentinite, clinopyroxenite, pegmatitic norite or INTRODUCTION...layered rocks of the DOI 10.1179/037174505X82152 cordierite spinel hornfels. The Main Zone differs mineralogically...sulphides than the Merensky Reef and UG-2 chromitite, a lower overall PGE grade in the mineralised zone which |  | | 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...the same kind contained in quartz-anthophyllite-cordierite rock; and later on he ran across so me more grains...zone and is characterized by amphibolites and cordierite-anthophyllite rocks intercalated with both skarn...minerals of Orijärvi occur in quartzanthophyllite-cordierite-biotite rocks as thin veinlets, the thickness |  | | 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...the same kind contained in quartz-anthophyllite-cordierite rock; and later on he ran across so me more grains...zone and is characterized by amphibolites and cordierite-anthophyllite rocks intercalated with both skarn...minerals of Orijärvi occur in quartzanthophyllite-cordierite-biotite rocks as thin veinlets, the thickness |  | 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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Lower serpentinite quarry, Zwettler Leiten, Felling, Gföhl, Krems-Land District, Lower Austria, Austria