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Molybdenite from
Rožná deposit, Rožná, Žďár nad Sázavou District, Vysočina Region, Czech Republic


Locality type:Deposit
Classification
Species:Molybdenite
Formula:MoS2
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Molybdenite data
Locality Data:Click here to view Rožná deposit, Rožná, Žďár nad Sázavou District, Vysočina Region, Czech Republic
Data Identifiers
Mindat Occurrence Record ID:430339
Long-form Identifier:1:3:430339:8
GUID (UUID V4):d8ba1381-e8f4-4e5c-9707-1c5eea3fcf87
Localities for Molybdenite in this Region
Rožná I Mine, Rožná deposit, Rožná, Žďár nad Sázavou District, Vysočina Region, Czech Republic
Nearest other occurrences of Molybdenite
0.1km (0.1 miles) Rožná I Mine, Rožná deposit, Rožná, Žďár nad Sázavou District, Vysočina Region, Czech Republic
30.2km (18.7 miles) Hedenbergite skarn, Svratouch, Chrudim District, Pardubice Region, Czech Republic
40.5km (25.2 miles) Borovina, Třebíč, Třebíč District, Vysočina Region, Czech Republic
42.1km (26.2 miles) Granite quarry, Pohled, Havlíčkův Brod District, Vysočina Region, Czech Republic
43.5km (27.0 miles) Litická quarry, Skuteč, Chrudim District, Pardubice Region, Czech Republic
53.5km (33.3 miles) Křižanovice deposit, Křižanovice, Chrudim District, Pardubice Region, Czech Republic
61.0km (37.9 miles) Orlík (Štůly), Humpolec, Pelhřimov District, Vysočina Region, Czech Republic
82.1km (51.0 miles) Nonndorf gabbro quarry, Nonndorf bei Raabs, Raabs an der Thaya, Waidhofen an der Thaya District, Lower Austria, Austria
84.3km (52.4 miles) Hengl quarry, Eibenstein an der Thaya, Raabs an der Thaya, Waidhofen an der Thaya District, Lower Austria, Austria
86.4km (53.7 miles) Kožušná (Fellberg), Maršíkov (Marchendorf), Velké Losiny, Šumperk District, Olomouc Region, Czech Republic
References
Reference Search (possible matching items)
Journal (article/letter/editorial)
1007/s00126-008-0188-0 ARTICLE The Rožná uranium deposit (Bohemian Massif, Czech Republic): shear zone-hosted, late...mineralization events are recorded at the Rožná uranium deposit (total mine production of 23,000 t U, average...K. Žák : P. Dobeš Czech Geological Survey, Klárov 3, 118 21 Prague 1, Czech Republic e-mail: kribek@cgu...Masaryk University, Kotlářská 2, 611 37 Brno, Czech Republic M. Pudilová Faculty of Sciences, Charles University...University, Albertov 6, 128 43 Prague 2, Czech Republic M. René Institute of Rock Structure and Mechanics
Journal (article/letter/editorial)
(Rytuba 2005). The world’s largest Hg deposit, the Almadén district of central Spain, is representative...reworking of the mercury-hosting rocks of the Almadén district (primary mineralization 427–380 Ma) led to at...associated with one larger contemporaneous mineralized region. Most notably, mindat.org records more than 300...west-central California. This important mining district, including the New Almadén mine in Santa Clara... and at Serra Pelada (Serra Leste) Au-(Pd-Pt) deposit, Pará, Brazil (Bindi 2010). However, we have not
Book (edition)
gangue mineral may be considered as waste in one deposit and as ore mineral in another (e.g., hedenbergite)...particular sample derives from the stockwork of such a deposit, it will normally contain amorphous silica/opal...in modern hydrothermal equivalents (e.g., JADE deposit, Okinawa Trough, Japan). Thus, metasomatic/metamorphic...mineral inventory available elsewhere. Further deposit descriptions originated from: binn.strahlen.org...Pressure twins are commonly found in graphite or molybdenite, where they are easily identified. Optical properties
Book
participants from 30 countries (e.g. Canada, China, Czech Republic, Russia, and United States) at TU Bergakademie...41 Uranium leaching from a burning black shale deposit – present conditions and future scenarios . . ...Molybdenum transfer within the oxidized zone of uranium deposit . . . . . . . . . . . . . . . . . . . . . . . ...heavily polluted drainage waters in a uranium deposit . . . . . . . . . . . . . . . . . . . . . . . ...Evolution at Abandoned Uranium Mines in the Czech Republic . . . . . . . . . . . . . . . . . . . . .
 
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