Multi-stage evolution of xenotime-(Y) from Písek pegmatites,
Czech Republic: an electron probe micro-analysis and Raman
spectroscopy study

J 2016

Multi-stage evolution of xenotime-(Y) from Písek pegmatites, Czech Republic: an electron probe micro-analysis and Raman spectroscopy study

ŠVECOVÁ, Eva; Renata ČOPJAKOVÁ; Zdeněk LOSOS; Radek ŠKODA; Lutz NASDALA et al.

Základní údaje

Originální název

Multi-stage evolution of xenotime-(Y) from Písek pegmatites, Czech Republic: an electron probe micro-analysis and Raman spectroscopy study

Autoři

ŠVECOVÁ, Eva; Renata ČOPJAKOVÁ; Zdeněk LOSOS; Radek ŠKODA; Lutz NASDALA a Jaroslav CÍCHA

Vydání

Mineralogy and Petrology, 2016, 0930-0708

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10500 1.5. Earth and related environmental sciences

Stát vydavatele

Rakousko

Utajení

není předmětem státního či obchodního tajemství

Impakt faktor

Impact factor: 1.236

Označené pro přenos do RIV

Ano

Kód RIV

RIV/00216224:14310/16:00090870

Organizační jednotka

Přírodovědecká fakulta

Klíčová slova česky

xenotim-(Y); vodné roztoky; metamiktizace; rekrystalizace; alterace; EPMA; Ramanova spektroskopie

Klíčová slova anglicky

xenotime-(Y); aqueous fluids; metamictization; recrystallization; alteration; EPMA; Raman spectroscopy

Štítky

AKR, rivok

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 3. 3. 2018 21:26, doc. RNDr. Zdeněk Losos, CSc.

Anotace

V originále

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.

Návaznosti

EE2.3.20.0052, projekt VaV

Název: Výzkumný tým pro ukládání radioaktivních odpadů a jadernou bezpečnost

Citovat

ŠVECOVÁ, Eva; Renata ČOPJAKOVÁ; Zdeněk LOSOS; Radek ŠKODA; Lutz NASDALA a 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, roč. 110, č. 6, s. 747-765. ISSN 0930-0708. Dostupné z: https://doi.org/10.1007/s00710-016-0442-6.

@article{1354605,
   author = {Švecová, Eva and Čopjaková, Renata and Losos, Zdeněk and Škoda, Radek and Nasdala, Lutz and Cícha, Jaroslav},
   article_number = {6},
   doi = {https://doi.org/10.1007/s00710-016-0442-6},
   keywords = {xenotime-(Y); aqueous fluids; metamictization; recrystallization; alteration; EPMA; Raman spectroscopy},
   language = {eng},
   issn = {0930-0708},
   journal = {Mineralogy and Petrology},
   title = {Multi-stage evolution of xenotime-(Y) from Písek pegmatites, Czech Republic: an electron probe micro-analysis and Raman spectroscopy study},
   volume = {110},
   year = {2016}
}

TY  - JOUR
ID  - 1354605
AU  - Švecová, Eva - Čopjaková, Renata - Losos, Zdeněk - Škoda, Radek - Nasdala, Lutz - Cícha, Jaroslav
PY  - 2016
TI  - Multi-stage evolution of xenotime-(Y) from Písek pegmatites, Czech Republic: an electron probe micro-analysis and Raman spectroscopy study
JF  - Mineralogy and Petrology
VL  - 110
IS  - 6
SP  - 747-765
EP  - 747-765
SN  - 09300708
KW  - xenotime-(Y)
KW  - aqueous fluids
KW  - metamictization
KW  - recrystallization
KW  - alteration
KW  - EPMA
KW  - Raman spectroscopy
N2  - 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.
ER  -

ŠVECOVÁ, Eva; Renata ČOPJAKOVÁ; Zdeněk LOSOS; Radek ŠKODA; Lutz NASDALA a Jaroslav CÍCHA. Multi-stage evolution of xenotime-(Y) from Písek pegmatites, Czech Republic: an electron probe micro-analysis and Raman spectroscopy study. \textit{Mineralogy and Petrology}. 2016, roč.~110, č.~6, s.~747-765. ISSN~0930-0708. Dostupné z: https://doi.org/10.1007/s00710-016-0442-6.

Přehled o publikaci