Petrogenesis of granitoids of the Červená type (Central Bohemian Plutonics Complex) = Petrogeneze granitoidů červenského typu (středočeský plutonický komplex)

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The Červená type granitoids are a part of a composite magmatic complex of Variscan age emplaces in a ductile shear zone on the boundary of the Bohemicum and the Moldanubian terranes. By their chemical composition, they areclosestto the hybrid granites (H-granites). Their origin is associated with the processes of mixing of the differentiated, high-potassium, mantle-derived magmas, assimilation with metavolcanics and metasediments of the upper crustand withsubsequent extensive homogenisation of the granitic melt … full description

Bibliographic Details

Main Author

Miloš René

Document Type

Articles

Physical Description

il.

Published in

Acta montana. Series A, Geodynamics. -- ISSN 1211-1910. -- č. 14(114) (1999), s. 81-97

Subjects

Česká republika > granitoidy > chemismus hornin > petrogeneze > tektonika zlomová > rudy U > Čechy