ŠVECOVÁ, Eva, Renata ČOPJAKOVÁ, Zdeněk LOSOS, Radek ŠKODA, Lutz NASDALA and Jaroslav CÍCHA. Multi-stage evolution of xenotime-(Y) from Písek pegmatites, Czech Republic: an electron probe micro-analysis and Raman spectroscopy study. Mineralogy and Petrology. 2016, vol. 110, No 6, p. 747-765. ISSN 0930-0708. Available from: https://dx.doi.org/10.1007/s00710-016-0442-6.
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Basic information
Original name Multi-stage evolution of xenotime-(Y) from Písek pegmatites, Czech Republic: an electron probe micro-analysis and Raman spectroscopy study
Authors ŠVECOVÁ, Eva (203 Czech Republic, belonging to the institution), Renata ČOPJAKOVÁ (203 Czech Republic, belonging to the institution), Zdeněk LOSOS (203 Czech Republic, guarantor, belonging to the institution), Radek ŠKODA (203 Czech Republic, belonging to the institution), Lutz NASDALA (40 Austria) and Jaroslav CÍCHA (203 Czech Republic).
Edition Mineralogy and Petrology, 2016, 0930-0708.
Other information
Original language English
Type of outcome Article in a journal
Field of Study 10500 1.5. Earth and related environmental sciences
Country of publisher Austria
Confidentiality degree is not subject to a state or trade secret
Impact factor Impact factor: 1.236
RIV identification code RIV/00216224:14310/16:00090870
Organization unit Faculty of Science
Doi http://dx.doi.org/10.1007/s00710-016-0442-6
UT WoS 000388834300004
Keywords (in Czech) xenotim-(Y); vodné roztoky; metamiktizace; rekrystalizace; alterace; EPMA; Ramanova spektroskopie
Keywords in English xenotime-(Y); aqueous fluids; metamictization; recrystallization; alteration; EPMA; Raman spectroscopy
Tags AKR, rivok
Tags International impact, Reviewed
Changed by Changed by: doc. RNDr. Zdeněk Losos, CSc., učo 2470. Changed: 3/3/2018 21:26.
Abstract
The chemical variability, degree of radiation damage, and alteration of xenotime from the Písek granitic pegmatites (Czech Republic) were investigated by micro-chemical analysis and Raman spectroscopy. Dominant large xenotime–(Y) grains enriched in U, Th and Zr crystallized from a melt almost simultaneously with zircon, monazite and tourmaline. Xenotime is well to poorly crystalline depending on its U and Th contents. It shows complex secondary textures cutting magmatic growth zones as a result of its interaction with F, Ca, alkali-rich fluids during the hydrothermal stage of the pegmatite evolution.
Links
EE2.3.20.0052, research and development projectName: Výzkumný tým pro ukládání radioaktivních odpadů a jadernou bezpečnost
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