Tectonometamorphic evolution of the Svratka Crystalline Complex (NE Bohemian Massif): Evidence for wrench-dominated transpression along the NE margin of the Variscan orogene root
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F06%3A00017227" target="_blank" >RIV/00216224:14310/06:00017227 - isvavai.cz</a>
Result on the web
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DOI - Digital Object Identifier
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Alternative languages
Result language
angličtina
Original language name
Tectonometamorphic evolution of the Svratka Crystalline Complex (NE Bohemian Massif): Evidence for wrench-dominated transpression along the NE margin of the Variscan orogene root
Original language description
Structural development of metagranites from considerred unit shows diferrent and anomalous deformation of feldspars vs. quartz. This feature is explained by polygonal recrystalization of feldspars and sliding along grain boundaries.
Czech name
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Czech description
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Classification
Type
O - Miscellaneous
CEP classification
DB - Geology and mineralogy
OECD FORD branch
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Result continuities
Project
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Continuities
Z - Vyzkumny zamer (s odkazem do CEZ)
Others
Publication year
2006
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů