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Publisher © Czech Geological Survey, ISSN: 2336-5757 (online), 0514-8057 (print)

Geological pattern of the Jindřichův Hradec district with great emphasis to the Kardašova Řečice area (Klenov Pluton, Moldanubian Batholith)

Kryštof Verner, Schulmannová Dudíková, Jakub Trubač, Jana Paclíková, Vojtěch Janoušek, Jaroslava Pertoldová, Vojtěch Janoušek

Geoscience Research Reports 43, 2010 (GRR for 2009), pages 81–83

Keywords: geochemistry, Bohemian Massif, Moldanubian Batholith, AMS, fabric, Klenov Pluton

Map sheets: Soběslav (23-31), Veselí nad Lužnicí (23-33)

Full text (PDF, 0.1 MB)

Abstract

We consider our preliminary results of petrochemical, structural and AMS analyses of granitoids of the Klenov Pluton located in eastern part of the Moldanubian Batholith. The Klenov Pluton has a peraluminous, high-K character formed by partial melting of a crustal metasedimentary (metapelite) source at relatively lower temperatures. In addition, the Klenov Pluton records a crucial role of magmatic stoping, regional HT-LP tectonometamorphic event during magma emplacement and crystallization.