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Contrasting tectonic evolution of gabbros of the MLC/TBU boundary, Bohemian Massif, CR
Petrological, geochemical and metamorphic characteristics of rocks of gabbroic protolith from the Mariánské Lázne Complex and from the NW. margin of the TBU were studied and compared....
DB - Geologie a mineralogie
- 1999 •
- D
Rok uplatnění
D - Stať ve sborníku
Silicified microbiota of the Neoproterozoic silicites of the Teplá-Barrandien area near the southeast margin of the Landscape Protected Area of Křivoklát in the Czech Republic
Neoproterozoic silicites from the Blovice Formation (Kralupy-Zbraslav Group, Teplá-Barrandian Unit) commonly contain microscopic organic remains. Two localities of silicites from the SE margin of the Landscape Protected Area of Křiv...
DB - Geologie a mineralogie
- 2009 •
- Jx
Rok uplatnění
Jx - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
Research of the crystalline formations in the deep structures underlay the Doupov complex and larger surroundings
Digital elevation model of crystalline basement and its geological structure below sedimentary and volcanics units in the area of Doupovské hory Mts. North Bohemian Basin and České středohoří Mts. was prepared on the basis evaluating the Geo...
DB - Geologie a mineralogie
- 2001 •
- Vx
Rok uplatnění
Vx - Nezařazeno - Výzkumná zpráva obsahující utajované informace (takový výsledek lze do RIV vložit pouze v případě, že zpráva obsahuje utajované informace a pole R12 = U), nebo souhrnná výzkumná zpráva
Teplá-Barrandian Unit (Moldanubian Zone)
Neoproterozoic stratigraphy, lithology, geochemistry of the Teplá-Barrandian Unit is characterized in the frame of Cadomian orogen.
DB - Geologie a mineralogie
- 2008 •
- C
Rok uplatnění
C - Kapitola v odborné knize
Character of the Contact between the Saxothuringian and Teplá-Barrandian Unit
Character of the Contact between the Saxothuringian and Teplá-Barrandian Unit;metamorphic zoning...
DB - Geologie a mineralogie
- 2003 •
- Jx
Rok uplatnění
Jx - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
Coronitic metagabbros of the Mariánské Lázně Complex and Teplá Crystalline Unit: inferences for the tectonometamorphic evolution of the western margin of the Teplá-Barrandian Unit, Bohemian Massif.
Interpretation of geological evolution of the unit using petrological, geochemical and mineralogical study of metagabbros and other metabasic rocks from MLC......
DB - Geologie a mineralogie
- 2002 •
- Jx
Rok uplatnění
Jx - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
Neoproterozoic of the Teplá-Barrandian Unit as a part of the Cadomian orogenic belt: A review and correlation aspects
?...
DB - Geologie a mineralogie
- 2000 •
- Jx
Rok uplatnění
Jx - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
Coronitic metagabbros of the Mariánské Lázně Complex and Teplá Crystalline Unit: inference fro the tectonometamorphic evolution of the western margin of the Teplá-Barrandian Unit, Bohemian Massif
Gochemistry, metamorphic evolution of metagabbross of the Early Palaeozoic Mariánské Lázně Complex were studied due to reconstruction of pre-Variscan and Variscan history of the teplá suture zone....
DB - Geologie a mineralogie
- 2002 •
- C
Rok uplatnění
C - Kapitola v odborné knize
Sources, emplacement environmnets, and metamorphic evolution of metagabbros in the Mariánské Lázně Complex and Teplá Crystalline Unit (NW Bohemian Massif).
Geological position and geochemistry of metabbross from the Mariánské Lázně Complex and Teplá Crystalline Unit is given and constraints for magma sources and emplacement environment are discussed....
DB - Geologie a mineralogie
- 2001 •
- Jx
Rok uplatnění
Jx - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
Explanation to the basic geological map of the Czech Republic in the scale 1:20 000, sheet 03-341 Kněžmost
The sheet area is formed of several unit of the Bohemian massif. The basement is formed of metamorphic complexes of Teplá- Barrandien and Lugikum units. The Permocarboniferous sequence of terrestrial clastic sedime...
DB - Geologie a mineralogie
- 2011 •
- O
Rok uplatnění
O - Ostatní výsledky
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