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2014•Unpublished venueRequires access

Behavior of B and Li during the evolution of the Kracovice pegmatite in respect to the tourmaline and garnet formation and stability

Renata Čopjaková, Radek Škoda, Michaela Vašinová Galiová, Milan Novák

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Abstract

Enrichment in B and Li is known from many evolved granites and pegmatites. The Kracovice pegmatite represents the most evolved body with mixed LCT-NYF signature related to the Třebic Pluton. We studied behavior of B and Li in respect to tourmaline and garnet. Minerals were analyzed by the Cameca SX100 electron microprobe. Lithium was determined using LA-ICP-MS (Department of Chemistry, Masaryk University, Brno).

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What this paper is about

Enrichment in B and Li is known from many evolved granites and pegmatites. The Kracovice pegmatite represents the most evolved body with mixed LCT-NYF signature related to the Třebic Pluton. We studied behavior of B and Li in respect to tourmaline and garnet. Minerals were analyzed by the Cameca SX100 electron microprobe. Lithium was determined using LA-ICP-MS (Department of Chemistry, Masaryk University, Brno).

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Available abstract

Enrichment in B and Li is known from many evolved granites and pegmatites. The Kracovice pegmatite represents the most evolved body with mixed LCT-NYF signature related to the Třebic Pluton. We studied behavior of B and Li in respect to tourmaline and garnet. Minerals were analyzed by the Cameca SX100 electron microprobe. Lithium was determined using LA-ICP-MS (Department of Chemistry, Masaryk University, Brno).

Key concepts: Tourmaline, Pegmatite, Electron microprobe, Geochemistry, Geology, EMPA, Mineralogy, Lithium (medication)

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Behavior of B and Li during the evolution of the Kracovice pegmatite in respect to the tourmaline and garnet formation and stability — Research Paper | ScholarLens