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 (203 Česká republika, domácí), Renata ČOPJAKOVÁ (203 Česká republika, domácí), Zdeněk LOSOS (203 Česká republika, garant, domácí), Radek ŠKODA (203 Česká republika, domácí), Lutz NASDALA (40 Rakousko) a Jaroslav CÍCHA (203 Česká republika)

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

Kód RIV

RIV/00216224:14310/16:00090870

Organizační jednotka

Přírodovědecká fakulta

DOI

http://dx.doi.org/10.1007/s00710-016-0442-6

UT WoS

000388834300004

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://dx.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 = {http://dx.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://dx.doi.org/10.1007/s00710-016-0442-6.

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