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Calcite from
Heroltice, Brno-Country District, South Moravian Region, Czech Republic


Locality type:Municipality
Classification
Species:Calcite
Formula:CaCO3
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Calcite data
Locality Data:Click here to view Heroltice, Brno-Country District, South Moravian Region, Czech Republic
Data Identifiers
Mindat Occurrence Record ID:510380
Long-form Identifier:1:3:510380:5
GUID (UUID V4):bfb4a3bd-71ef-44c8-84b8-06f2bb49a50c
References
Reference Search (possible matching items)
Journal (article/letter/editorial)
Journal of the Czech Geological Society 51/3–4(2006) 189 Želetice Group: Very low-grade Palaeozoic...Palaeozoic sequence at the base of Moravicum, Czech Republic Želetická skupina: velmi nízce metamorfovaná paleozoická...Department of Geological Sciences PøF MU Brno, Kotláøská 2, 611 37 Brno; Leichman@sci.muni.cz We define a...that crops out in the northern termination of the Moravian Dyje window and in the central part of the Svratka...window in the hanging wall of the Devonian Lažánky-Heroltice limestones and below the biotite-bearing phylites
Book
and N. M. BANAS, W. KRAMER, VII Moldanubian Region VII.A Introduction J. FIALA. . . . and K. VII...Contributors J. AICHLER Czech Geological Survey P.O. Box 65 79001 Jesenik Czech Republic H.-J. ANDERLE Geological...Charles University Albertov6 12843 Prague 2 Czech Republic I. CHLUPAc Department of Geology Faculty of...Charles University Albertov 6 12843 Prague 2 Czech Republic R.D. DALLMEYER Department of Geology University...DUDEK J. CHAB Czech Geological Survey Malostranske mlm. 19 11821 Prague 1 Czech Republic Department of
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...(Franciscan Formation in California) and in the west of South America; relicts are preserved in the Alps and probably...1600°C (Bentor and Kastner, 1976) so that the country rocks are recrystallized or partly fused over areas...(after Zoubek 1948) in this book as a metamorphic region, and a set of metamorphic regions which belong
 
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