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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Europe
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Carpathians
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Slovakian Carpathians
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Spis-Gemer (1)
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Western Carpathians (3)
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Central Europe
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Slovakia
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Slovakian Carpathians
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Spis-Gemer (1)
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Veporides (1)
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commodities
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metal ores
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rare earth deposits (1)
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uranium ores (1)
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mineral deposits, genesis (2)
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elements, isotopes
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metals
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actinides
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uranium (1)
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antimony (1)
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bismuth (1)
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iron
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ferric iron (1)
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rare earths
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gadolinium (2)
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geologic age
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Paleozoic
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Gemericum (1)
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Permian (1)
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igneous rocks
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igneous rocks
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plutonic rocks
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granites
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aplite (1)
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metamorphic rocks
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metamorphic rocks
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gneisses
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orthogneiss (1)
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minerals
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arsenates
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scorodite (1)
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carbonates
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cerussite (1)
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oxides
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brannerite (1)
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uraninite (1)
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phosphates
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autunite (1)
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fluorapatite (1)
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monazite (2)
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xenotime (2)
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sulfides
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galena (1)
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uranium minerals (2)
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Primary terms
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crystal chemistry (2)
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crystal structure (2)
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Europe
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Carpathians
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Slovakian Carpathians
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Spis-Gemer (1)
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Western Carpathians (3)
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Central Europe
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Slovakia
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Slovakian Carpathians
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Spis-Gemer (1)
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Veporides (1)
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-
-
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ground water (1)
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igneous rocks
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plutonic rocks
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granites
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aplite (1)
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intrusions (1)
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metal ores
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rare earth deposits (1)
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uranium ores (1)
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metals
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actinides
-
uranium (1)
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-
antimony (1)
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bismuth (1)
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iron
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ferric iron (1)
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-
rare earths
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gadolinium (2)
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-
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metamorphic rocks
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gneisses
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orthogneiss (1)
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-
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metasomatism (2)
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mineral deposits, genesis (2)
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Paleozoic
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Gemericum (1)
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Permian (1)
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Xenotime-(Gd), a new Gd-dominant mineral of the xenotime group from the Zimná Voda REE–U–Au quartz vein, Prakovce, Western Carpathians, Slovakia
Secondary uranyl arsenates–phosphates and Sb–Bi-rich minerals of the segnitite–philipsbornite series in the oxidation zone at the Prakovce-Zimná Voda REE–U–Au quartz-vein mineralisation, Western Carpathians, Slovakia
Monazite-(Gd), a new Gd-dominant mineral of the monazite group from the Zimná Voda REE–U–Au quartz vein, Prakovce, Western Carpathians, Slovakia
Gadolinium-dominant monazite and xenotime: Selective hydrothermal enrichment of middle REE during low-temperature alteration of uraninite, brannerite, and fluorapatite (the Zimná Voda REE-U-Au quartz vein, Western Carpathians, Slovakia)
Permian lamprophyres from the Western Carpathians: a review
Abstract Calc-alkaline lamprophyres from the Western Carpathians occur as dykes and sills in the crystalline complexes (predominantly granites and gneisses) of the Tatric Unit. Some of the lamprophyre dykes have been strongly overprinted by tectonism and hydrothermal fluid ingress. They have a similar mineralogical composition, and they are comprised of clinopyroxene, amphibole, biotite and plagioclase. Based on their modal composition, they can be classified as spessartites and kersantites, and based on their geochemical composition, most of them are of calc-alkali type. Lamprophyres from individual core complexes (e.g. the Malá Fatra Mountains and Nízke Tatry Mountains) exhibit variable Nb, Ta and Sr–Nd isotope signatures. These differences are probably due to compositional variations in the mantle source and/or the lower crust at the site of lamprophyre melt generation, or variable incorporation of crustal material. The age of the lamprophyres is Permian ( c. 265 Ma) based on U–Pb LA-ICP-MS dating of apatite micro-phenocrysts.