Locality type: | Vein |
Classification |
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Species: | Calcite |
Formula: | CaCO3 |
Confirmation |
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Validity: | Believed Valid |
Data |
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Mineral Data: | Click here to view Calcite data |
Locality Data: | Click here to view S1 vein, Radětice shaft, Radětice, Příbram District, Central Bohemian Region, Czech Republic |
Data Identifiers |
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Mindat Occurrence Record ID: | 1604190 |
Long-form Identifier: | 1:3:1604190:1 |
GUID (UUID V4): | 053bc1f2-c243-4ede-a265-d5a15a1992a3 |
Nearest other occurrences of Calcite |
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4.6km (2.9 miles) | ⓘUranium Mine No. 68 (Shaft No. 68), Milín, Příbram District, Central Bohemian Region, Czech Republic |
4.6km (2.9 miles) | ⓘMine dump, Uranium Mine No. 16, Háje, Příbram District, Central Bohemian Region, Czech Republic |
4.8km (3.0 miles) | ⓘUranium Mine No. 16, Háje, Příbram District, Central Bohemian Region, Czech Republic |
4.9km (3.1 miles) | ⓘAlexander Mine, Vrančice, Příbram District, Central Bohemian Region, Czech Republic |
5.0km (3.1 miles) | ⓘVáclav shaft (Václav mine), Vrančice, Příbram District, Central Bohemian Region, Czech Republic |
5.3km (3.3 miles) | ⓘUranium Mine No. 9 (Shaft No. 9), Háje, Příbram District, Central Bohemian Region, Czech Republic |
5.3km (3.3 miles) | ⓘUranium Mine No. 21, Dubno, Příbram District, Central Bohemian Region, Czech Republic |
5.7km (3.6 miles) | ⓘUranium Mine No. 4 (Shaft No. 4), Lešetice, Příbram District, Central Bohemian Region, Czech Republic |
5.8km (3.6 miles) | ⓘB117 hydrothermal vein, Uranium Mine No. 6 (Shaft No. 6), Brod, Příbram, Příbram District, Central Bohemian Region, Czech Republic |
8.2km (5.1 miles) | ⓘProkop Mine, Březové Hory deposit, Březové Hory, Příbram, Příbram District, Central Bohemian Region, Czech Republic |
References |
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Sejkora, Jiřı́, Biagioni, Cristian, Škácha, Pavel, Musetti, Silvia, Kasatkin, Anatoly V, Nestola, Fabrizio (2023) Tetrahedrite-(Cd), Cu 6 (Cu 4 Cd 2) Sb 4 S 13, from Radětice near Přı́bram, Czech Republic: the new Cd member of the tetrahedrite group. European Journal of Mineralogy, 35 (6) 897-907 |
Reference Search (possible matching items) |
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| Acosta-Góngora, P., Gleeson, S.A., Samson, I.M., Corriveau, L., Ootes, L., Taylor, B.E., Creaser, R.A., Muehlenbachs, K. (2015) Genesis of the Paleoproterozoic NICO iron oxide–cobalt–gold–bismuth deposit, Northwest Territories, Canada: Evidence from isotope geochemistry and fluid inclusions. Precambrian Research, 268. 168-193 doi:10.1016/j.precamres.2015.06.007 | Journal (article/letter/editorial) | by a set of pre-ore quartz ± calcite + amphibole + Kfeldspar veins (S1). The Co–Au–Bi (±W–Cu–Mo) mineralization...origin of the fluids. Two out of three calcite samples from pre-(S1) and post-ore (S3) veins have also ␦13...magmatic origin (−5.5 to −3.6‰). However, one calcite sample from the S3 veins has a value that indicates...GBMZ rocks. The quartz ␦18 O values suggest that S1 (12.7‰) formed at higher temperatures than S2 (13...equilibration. Secondary trails of native Bi in S1 vein quartz are associated with liquid–vapor (LV) and | | | Journal (article/letter/editorial) | studies of early Variscan mineralisation and Pb-Sb vein deposits in the Cornubian ore®eld: implications...Basin (SW England) contain stratiform and Pb-Sb vein deposits that reveal a wide variation in d34S and...individual vein parageneses and depletion of the ¯uid sulphur reservoir during evolution of the vein systems...brittle deformation was an important mechanism for vein carbonation. An origin for the Pb-Sb mineralisation...chemical and ¯uid inclusion data for the Trevone vein mineralisation identi®ed distinct SbAs-(Au) and | | | Journal (article/letter/editorial) | scale of 1:600 in severalother early dikes in the central portion of an areaeastof the Sericitefault (Fig...previously mentioned units. These district, Lyon County, Nevada. The district lies 80 dikesare thoughtto be...biotite) alterationof Nevadastocksintruded the central portionsof the batholith. Empire porphyrydikesin...Walker ment of granite porphyry dikes in the west-central River porphyrydikes(Fig. 3B) wasalsoaccompanied...most intense sodium- Quartz 60 K-feldspar _J Vein Plagioclase o 1501 calciummetasomatism is adjacentto | | Fourcade, Serge, Trotignon, Laurent, Boulvais, Philippe, Techer, Isabelle, Elie, Marcel, Vandamme, Didier, Salameh, Elias, Khoury, Hani (2007) Cementation of kerogen-rich marls by alkaline fluids released during weathering of thermally metamorphosed marly sediments. Part I: Isotopic (C,O) study of the Khushaym Matruk natural analogue (central Jordan) Applied Geochemistry, 22 (7) 1293-1310 doi:10.1016/j.apgeochem.2007.02.012 | Journal (article/letter/editorial) | study of the Khushaym Matruk natural analogue (central Jordan) Serge Fourcade a,*, Laurent Trotignon b...March 2007 Abstract The Khushaym Matruk site in central Jordan may represent a natural analogue depicting...thermodynamic approach of the alteration parageneses (calcite–jennite–afwillite–brucite and CSH phases) in the... Se a The Khushaym Matruk site is located in Central Jordan, at about 80 km SE of Amman in a desert...Sketch location map of the Khushaym Matruk site in central Jordan. The Maqarin site, located in northern Jordan | | | Journal (article/letter/editorial) | Act: actinolite, Alln: allanite, Ap: apatite, Cc: calcite, Chl: chlorite, Car: Fe-Mg carpholite, Crs: crossite...area into three thrust-bounded regions (Fig. 1). Region I, consists of a tectonic mélange metamorphosed... serpentinites and basalts (Hawasina Complex). Region II, consists of several thrust sheets of folded...epidote-blueschist facies conditions. The structurally lowest Region III is predominated by calcareous mica schists...grade from epidote-blueschist facies conditions in central Saih Hatat (zone A of El-Shazly et al., 1990) to | | | Journal (article/letter/editorial) | of veining.Silicificationand albitizationof the vein wall rock increasedits competence,and furtherfr...120ø but with variableaxialplanes. Descriptionof Vein Types Manyquartz-carbonate veins(up to i m long)were...DA VISON (o) (c) © © (d) FIG. 9. Details of vein geometries.(a). Early quartz-carbonateveinsfolded...deformations;5-m level, body C. (b). Concordant(with S1) vein with a symmetricregular alterationhalo which wasfolded...(1) concordant with S• cut by a discordantquartz vein (2); both are cut by an arsenopyritevein (3) which |
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