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2. ) metasediments. 3. Central Bohemian Pluton (mostly Sázava Tonalite, Blatná Granodiorite and the Marginal Granite. Contact aureole: Variscan contact metamorphism (the Central Bohemian Pluton). Mineralization: 1. stratiform mineralization connected with the volcanic members (pyrite and Cu, Zn sulphides, 2. vein and stockwork style of the Au-quartz, scheelite and Ag-polymetallic and barite mineralization. Fig. 14.. Jílové Volcanic Belt geological sketchmap (adapted after Morávek et al. 1994). 1 – Jílové Alaskite (Albite Granite), Trondhjemite, Metatonalite, 2 – Jílové Orthogneiss, 3 – Jílové Metavolcanites, 4 – Variscan biotite granite, 5 – faults.

Stř. Úst. geol. 61, 5, 265–272. 34 KETTNER, R. (1952): Geology of Třemšín unit and its surroundings. – Věst. Král. Čes. Společ. Nauk, T. mat-přírodověd. 14, 1–21. (Czech) ZACHARIÁŠ, J. (2008): Compositional trends in magmatic and hydrothermal silicates of the Petráčkova hora intrusive complex, Bohemian Massif – link between the magmatic processes and intrusion-related gold mineralization. – J. Geosci. 53, 105–117. ZACHARIÁŠ, J. – PERTOLD, Z. – PUDILOVÁ, M. – ŽÁK, K. – PERTOLDOVÁ, J. – STEIN, H.

Mineralization: not reported. Regional position: a member of the Proterozoic basement in the belt between the Ondřejov and Chocerady roof pendants of the CBP. Rock types: Ondřejov Metatonalite – sheared or foliated biotite metatonalite and hornblendebiotite metatonalite (two facies). Size and shape (in erosion level): outcrop of 400 × 200 m in size. References VAJNER, V. (1963): Geologie metamorfovaného ostrova ondřejovského. – Sbor. geol. Věd, Geol. 1, 21–41. VRÁNA, S. (1981): Metatonalite-metaconglomerate relation: the problem of the Upper Proterozoic sequence and its basement in the NE part of the Central Bohemian Pluton.

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