| Locality type: | Mine |
| Classification |
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| Species: | Talc |
| Formula: | Mg3Si4O10(OH)2 |
| Confirmation |
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| Validity: | Believed Valid |
| Data |
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| Mineral Data: | Click here to view Talc data |
| Locality Data: | Click here to view Lassing talc mine, Lassing, Liezen District, Styria, Austria |
| Data Identifiers |
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| Mindat Occurrence Record ID: | 265673 |
| Long-form Identifier: | 1:3:265673:1 |
| GUID (UUID V4): | c63fd621-9f30-4031-9296-0ed094c4fa63 |
| Nearest other occurrences of Talc |
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| 19.0km (11.8 miles) | ⓘMagnesite deposit, Sunk, Hohentauern, Murtal District, Styria, Austria |
| 28.4km (17.6 miles) | ⓘGypsum mine, Wienern, Grundlsee, Liezen District, Styria, Austria |
| 31.1km (19.3 miles) | ⓘMagnesite mine, Wald am Schoberpass, Leoben District, Styria, Austria |
| 43.0km (26.7 miles) | ⓘSchwarzenberg quarry (Katsch quarry), Katsch an der Mur, Teufenbach-Katsch, Murau District, Styria, Austria |
| 45.3km (28.2 miles) | ⓘTalc mine, Mautern in Steiermark, Leoben District, Styria, Austria |
| 49.9km (31.0 miles) | ⓘBodenmoosgraben talc mine, Lessach, Tamsweg District, Salzburg, Austria |
| 50.0km (31.1 miles) | ⓘStyrian Erzberg, Eisenerz, Leoben District, Styria, Austria |
| 62.5km (38.9 miles) | ⓘLeucophyllite mine, Kothgraben (Kotgraben), Kleinfeistritz, Weißkirchen in Steiermark, Murtal District, Styria, Austria |
| 63.3km (39.3 miles) | ⓘLobminggraben quarry, Lobminggraben, Sankt Stefan ob Leoben, Leoben District, Styria, Austria |
| 63.7km (39.6 miles) | ⓘStegsdorf, Sankt Salvator, Friesach, Sankt Veit an der Glan District, Carinthia, Austria |
| References |
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| Reference Search (possible matching items) |
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 | | Journal (article/letter/editorial) | | magnesites and dolomites at the Oberdorf/Laming (Austria) deposit and implications for their origin By WOLFGANGKIESL...alternating rock masses at the Oberdorf/Laming (Styria, Austria) mineralization has been studied. The rare...Universidit Wien, Dr:Karl-Lueger-Ring 1, A-1010 Wien, Austria. Manuscript received: 3.5.89; accepted: 5.2.90...times of these elements in seawater. Analyses of talc pseduomorphs after magnesite indicate as well that...serpentinites below the gneiss complexes of eastern Styria and the South Penninic units of the Tauern window |
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