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TŘEBÍČ, WESTERN CONTACT OF THE TŘEBÍČ PLUTON AND MOLDANUBICUM

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MELICHAR Rostislav HRDLIČKOVÁ Kristýna MAREČEK Lukáš BÁRTA František HOLUB František

Rok publikování 2019
Druh Článek ve sborníku
Fakulta / Pracoviště MU

Přírodovědecká fakulta

Citace
www Celý sborník ke stažení.
Popis A long outcrop situated next to the Sucheniova St. shows the character of the western edge of the Třebíč Pluton with its Moldanubian host rocks (Fig. 12-1). Country rocks of the western margin of the Třebíč Pluton are represented by migmatized biotite paragneiss to stromatitic migmatite of the Moldanubian Monotonous Group, commonly cordierite-bearing, sporadically, and only locally, also sillimanite and exceptionally garnet were described in this rock (Kala – Lacinová 1990). The dominant igneous rocks of Třebíč Pluton are coarse-grained Kfs-phyric amphibole–biotite melagranite to quartz syenite (‘durbachite’). Other rock types of the Třebíč Pluton are less common and are represented by the so-called “marginal facies” of syenite to granite and biotite granite.