 | | Journal (article/letter/editorial) | | evolution of an ore district illustrated—4D-animation from the Skellefte district, Sweden—Pietari Skyttä...polymetallic ore deposit, Podrinje metallogenic district, Serbia: Compositional variations and zoning—Slobodan...Recent massive sulfide deposits of the Semenov ore district, MidAtlantic Ridge, 13°31' N: Associated rocks...Le-Bing Fu Synmetamorphic carbon mobility and graphite enrichment in metaturbidites as a precursor to...Horní Slavkov-Krásno Sn-W ore district, Bohemian massif, Czech Republic—Zdeněk Dolníček, Miloš René |  | Finger, F., Gerdes, A., Janoušek, V., René, M., Riegler, G. (2007) Resolving the Variscan evolution of the Moldanubian sector of the Bohemian Massif: the significance of the Bavarian and the Moravo-Moldanubian tectonometamorphic phases. Journal of GEOsciences, 52 (1-2) 9-28 | Journal (article/letter/editorial) | | Frankfurt, Germany 3 Czech Geological Survey, Klárov 3, 118 21 Prague 1, Czech Republic 4 Academy of Sciences...Mechanics, V Holešovičkách 41, 182 09 Prague 8, Czech Republic * Corresponding author 1 2 The Variscan evolution...Moravo–Moldanubian Fold Belt can be followed from the Czech Republic southwards into eastern Bavaria and western...lithological links between the Moldanubian Zone in the Czech Republic and the Moldanubian Zone in Bavaria. The outcome...Massif (Moldanubian s. s.) covers essentially the region between the Teplá–Barrandian Unit in the north-west |  | | Book | | Jarchovský Govind S. Rajpoot Czech Geological Survey Prague 2010 CZECH GEOLOGICAL SURVEY ATLAS of plutonic...Waste Repository Authority of the Czech Republic (RAWRA) and by the Czech Geological Survey. Acknowledgements...author Josef Klomínský, Czech Geological Survey, Klárov 131/3, Prague 1, Czech Republic. Fax (+420) 257 531...b a Czech Geological Survey, Klárov 131/3, Praha 1, b Náchodská 2030, Praha 9, Czech Republic Contents...PLUTON (CBP) ……………………………………………………...16 1.01.1. KLATOVY MASSIF........................................ |  | Houzar, S., Litochleb, J., Sejkora, J., Cempírek, J., Cícha, J. (2008) Unusual mineralization with niobian titanite and Bi-tellurides in scheelite skarn from Kamenné doly quarry near Písek, Moldanubian Zone, Bohemian Massif. Journal of GEOsciences, 53 (1) 1-16 | Journal (article/letter/editorial) | | Moravian Museum, Zelný trh 6, 659 37 Brno, Czech Republic; shouzar@mzm.cz Department of Mineralogy and...79 Prague 1, Czech Republic Prácheň Museum, Velké náměstí 114, 397 24 Písek, Czech Republic Corresponding...Complex. In addition there are minor domains of graphite quartzite and marble enclosed in biotite gneiss...Geological sketch of the Písek area (modified from the Czech Geological Survey map 1:50 000). small dykes of...the joint facility of the Masaryk University and Czech Geological Survey in Brno; operator R. Škoda). The |  | | Book | | especially to Mrs. H. Zárubová who translated the Czech text, and to Mrs. M. Holubová and J. Maasová for...degree be analogous to the metamorphism of. another region but it is unique and unrepeatable in the combination...(after Zoubek 1948) in this book as a metamorphic region, and a set of metamorphic regions which belong...example of the model grid is the one computed for the region of sillimanite isograd 2 with the use of empiric...geological scale in the Crystalline of the Krušné hory Mts. (Mathé, 1976). It is not only alkalies that |  | Majzlan, J., Lalinska, B., Chovan, M., Blass, U., Brecht, B., Gottlicher, J., Steininger, R., Hug, K., Ziegler, S., Gescher, J. (2011) A mineralogical, geochemical, and microbiogical assessment of the antimony- and arsenic-rich neutral mine drainage tailings near Pezinok, Slovakia. American Mineralogist, 96 (1) 1-13 doi:10.2138/am.2011.3556 | Journal (article/letter/editorial) | | residua consisted of quartz with a minor amount of graphite, as shown by X-ray diffraction analyses. The X-ray...Advance diffractometer, employing CuKα radiation, graphite secondary-radiation monochromator, and a scintillation...(cf. Heikkinen et al. energy steps of 5 eV in the region from –150 to –50 eV relative to the absorption...Lindsay et al. 2009). edge,Fig. of 2 eV1. in the region from –50 to –20 eV, of 0.5 eV from –20 to +20 eV...anthropogenic deposits at the Mokrsko, Roudný, and Kašperské Hory gold deposits, Bohemian Massif (Cz). Environmental |
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