Locality type: | Area |
Classification |
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Species: | Muscovite |
Formula: | KAl2(AlSi3O10)(OH)2 |
Confirmation |
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Validity: | Believed Valid |
Data |
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Mineral Data: | Click here to view Muscovite data |
Locality Data: | Click here to view Thermal springs area, Karlovy Vary, Karlovy Vary District, Karlovy Vary Region, Czech Republic |
Data Identifiers |
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Mindat Occurrence Record ID: | 1004328 |
Long-form Identifier: | 1:3:1004328:0 |
GUID (UUID V4): | 29ed33f6-f7f2-4d5a-a67d-200848fa0b86 |
Nearest other occurrences of Muscovite |
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13.1km (8.1 miles) | ⓘKrudum granite body, Třídomí, Horní Slavkov, Sokolov District, Karlovy Vary Region, Czech Republic |
13.7km (8.5 miles) | ⓘVykmanov, Ostrov, Karlovy Vary District, Karlovy Vary Region, Czech Republic |
16.1km (10.0 miles) | ⓘSvornost Mine, Jáchymov, Karlovy Vary District, Karlovy Vary Region, Czech Republic |
18.0km (11.2 miles) | ⓘJeroným Mine, Čistá, Rovná, Sokolov District, Karlovy Vary Region, Czech Republic |
20.4km (12.7 miles) | ⓘMeluzína hill, Krásný Les, Karlovy Vary District, Karlovy Vary Region, Czech Republic |
23.8km (14.8 miles) | ⓘVykmanov, Perštejn, Chomutov District, Ústí nad Labem Region, Czech Republic |
25.2km (15.7 miles) | ⓘŠindelová, Sokolov District, Karlovy Vary Region, Czech Republic |
27.4km (17.1 miles) | ⓘMagnetite Mine, Měděnec, Chomutov District, Ústí nad Labem Region, Czech Republic |
27.6km (17.1 miles) | ⓘStraßburger Glück Mine, Niederschlag, Bärenstein, Erzgebirgskreis, Saxony, Germany |
28.5km (17.7 miles) | ⓘTisová, Kraslice, Sokolov District, Karlovy Vary Region, Czech Republic |
References |
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Reference Search (possible matching items) |
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| | Journal (article/letter/editorial) | fluxes: Quantitative constraints from hydrothermal springs John A. Becker, Mike J. Bickle ⁎, Albert Galy,...November 2007 Editor: R.W. Carlson Abstract Hot springs in the Marsyandi Valley, Nepal, vent CO2 sourced...Himalaya; CO2; metamorphism; carbon cycle; hot springs; climate; isotopes 1. Introduction An important...geochemistry and stable isotopes of Himalayan hot springs to determine CO2 fluxes in the Marsyandi Valley...been based on dissolved inorganic carbon in hot springs. Calculations of the contribution of metamorphic | | | Report (issue) | miles north of the Thelon River in the Mackenzie District of the Northwest Territories of Canada has a carbon-14...500 ± 250 yr, coinciding with the postglacial thermal maximum. Neither the pingo nor the silt of which...considerations it is evident that the surrounding area was freed of ice considerably more than 5,500 years...marked cooling of climate following the postglacial thermal maximum. Organic materials have also been found...groups (Dev&n and Cornwall; northern Pennines; Lake District; Harlech and Aberystwyth, North Wales; and Abergairn | | Brenot, Agnès, Cloquet, Christophe, Vigier, Nathalie, Carignan, Jean, France-Lanord, Christian (2008) Magnesium isotope systematics of the lithologically varied Moselle river basin, France. Geochimica et Cosmochimica Acta, 72 (20) 5070-5089 doi:10.1016/j.gca.2008.07.027 | Journal (article/letter/editorial) | HYDROLOGY AND GEOLOGY The Moselle River basin (surface area = 3080 km2) is located in northeastern France (Fig...K-Feldspar and muscovite granites; (2) Type II: Plagioclase predominating over K-feldspar and muscovite granite...Maxonchamp (Fig. 1), representing 18% of the surface area); (3) Type III: Biotite and hornblende bearing granites...Moselotte sub-basin, representing 45% of the surface area). This part of the basin is characterized by low...permeability layers and to the main aquifer system of the area, and inputs to the Moselle River mainly occur by | | Oliver, Lee, Harris, Nigel, Bickle, Mike, Chapman, Hazel, Dise, Nancy, Horstwood, Matthew (2003) Silicate weathering rates decoupled from the 87Sr/86Sr ratio of the dissolved load during Himalayan erosion. Chemical Geology, 201 (1) 119-139 doi:10.1016/s0009-2541(03)00236-5 | Journal (article/letter/editorial) | is necessary to show that the Himalayan –Tibet region is weathering silicate rocks at a significantly...Chemical Geology 201 (2003) 119–139 Himalayan – Tibet region does contribute major cation and Sr fluxes that...by Evans et al. (2001) who concluded that hot springs are major contributors of radiogenic Sr to Himalayan...Sr/86Sr values were obtained using a VG Sector 54 thermal ionisation mass spectrometer (TIMS) at the Department...by BK in Table 1. Box indicates detailed sampling area (Fig. 3). of 40 Am. Data were normalised to an | | | Book | focuses attention on the caves associated with the springs which are described in Chap. 4. Then, the tale...respectively. The northern hydrologic boundary of the area discussed here is the Bullpasture River, a tributary...the northern boundary and is the location of the springs that drain the caves of Burnsville Cove. Route...Burnsville (Fig. 1.3). The southern limit of the Karst area is about a mile south of Burnsville. Burnsville...provides outlets for the water as a series of springs. The result is that the downstream reaches of the |
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