2017Unpublished venueRequires access

Tourmalines of the eastern part of the Bohemian Massif

David Buriánek, Jan Cempírek, Renata Čopjaková, Jakub Haifler, Stanislav Houzar, Sebastián Hreus, Jan Loun, Jan Kocáb, Lukáš Krmíček, Radek Škoda, Jiřı́ Toman, Robert Trumbull, Michaela Vašinová Galiová, Adam Zachař, Petr Gadas, Milan Novák

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Abstract

Tourmaline-supergroup minerals are found in a large variety of igneous, metamorphic, hydrothermal and sedimentary rocks. Eastern border of the Bohemian Massif (contact of the Moldanubian Zone, Svratka Unit, and the Moravo-Silesian Zone of the Brunovistulian terrane) has extremely variable geology with tourmaline occurrences in granites, marbles, mica schists (tourmalinites), orthogneisses (tin-bearing metagranites), skarns, pegmatites, granulites, migmatites, and hydrothermal veins. This book provides an introduction to the geological evolution of the area and tourmaline occurrences; it is aimed as a field-trip guidebook for specialists in tourmaline petrology and mineralogy.

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What this paper is about

Tourmaline-supergroup minerals are found in a large variety of igneous, metamorphic, hydrothermal and sedimentary rocks. Eastern border of the Bohemian Massif (contact of the Moldanubian Zone, Svratka Unit, and the Moravo-Silesian Zone of the Brunovistulian terrane) has extremely variable geology with tourmaline occurrences in granites, marbles, mica schists (tourmalinites), orthogneisses (tin-bearing metagranites), skarns, pegmatites, granulites, migmatites, and hydrothermal veins. This book provides an introduction to the geological evolution of the area and tourmaline occurrences; it is aimed as a field-trip guidebook for specialists in tourmaline petrology and mineralogy.

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Available abstract

Tourmaline-supergroup minerals are found in a large variety of igneous, metamorphic, hydrothermal and sedimentary rocks. Eastern border of the Bohemian Massif (contact of the Moldanubian Zone, Svratka Unit, and the Moravo-Silesian Zone of the Brunovistulian terrane) has extremely variable geology with tourmaline occurrences in granites, marbles, mica schists (tourmalinites), orthogneisses (tin-bearing metagranites), skarns, pegmatites, granulites, migmatites, and hydrothermal veins. This book provides an introduction to the geological evolution of the area and tourmaline occurrences; it is aimed as a field-trip guidebook for specialists in tourmaline petrology and mineralogy.

Key concepts: Tourmaline, Geology, Massif, Geochemistry, Hornfels, Metamorphic rock, Granulite, Pegmatite

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