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- W4214906768 abstract "The Central Bohemian magmatic complex belongs to the Central European Variscan belt. The granitic rocks of this plutonic complex are formed by several suites of granites, granodiorites, and tonalites, together with small bodies of gabbros, gabbro diorites, and diorites. The granodiorites of the Blatná suite are high-K, calc-alkaline to shoshonitic, and metaluminous to slightly peraluminous granitic rocks. Compared to the common I-type granites, granodiorites of the Blatná suite are enriched in Mg (1.0–3.4 wt.% MgO), Ba (838–2560 ppm), Sr. (257–506 ppm), and Zr (81–236 ppm). For granodiorites of the Blatná suite is assemblage of apatite, zircon, titanite, and allanite significant. Zircon contains low Hf concentrations (1.1–1.7 wt.% HfO2). The composition of titanite ranges from 83 to 92 mol.% titanite end-member. Allanite is relatively Al-poor and displays Feox. ratio 0.2–0.5." @default.
- W4214906768 created "2022-03-05" @default.
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- W4214906768 date "2022-02-22" @default.
- W4214906768 modified "2023-09-26" @default.
- W4214906768 title "Investigation of Accessory Minerals from the Blatná Granodiorite Suite, Bohemian Massif, Czech Republic" @default.
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- W4214906768 doi "https://doi.org/10.5772/intechopen.102628" @default.
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