Geochemistry of Y plus REE in stratiform tourmalinites and
their tourmalines: implications for their genesis

D 2013

Geochemistry of Y plus REE in stratiform tourmalinites and their tourmalines: implications for their genesis

ČOPJAKOVÁ, Renata, Radek ŠKODA, Milan NOVÁK a Michaela VAŠINOVÁ GALIOVÁ

Základní údaje

Originální název

Geochemistry of Y plus REE in stratiform tourmalinites and their tourmalines: implications for their genesis

Název česky

Geochemie Y+REE ve stratiformních turmalinitech a jejich turmalínech: implikace pro jejich genezi

Autoři

ČOPJAKOVÁ, Renata (203 Česká republika, domácí), Radek ŠKODA (203 Česká republika), Milan NOVÁK (203 Česká republika) a Michaela VAŠINOVÁ GALIOVÁ (203 Česká republika)

Vydání

UPPSALA, MINERAL DEPOSIT RESEARCH FOR A HIGH-TECH WORLD, VOLS. 1-4, od s. 1705-1708, 4 s. 2013

Nakladatel

SGU-SVERIGES GEOLOGISKA UNDERSOKNING-GEOLOGY SURVEY SWEDEN

Další údaje

Jazyk

angličtina

Typ výsledku

Stať ve sborníku

Obor

10500 1.5. Earth and related environmental sciences

Stát vydavatele

Švédsko

Utajení

není předmětem státního či obchodního tajemství

Forma vydání

tištěná verze "print"

Kód RIV

RIV/00216224:14310/13:00066875

Organizační jednotka

Přírodovědecká fakulta

ISBN

978-91-7403-207-9

UT WoS

000337983900431

Klíčová slova anglicky

Y plus REE; tourmaline; stratiform tourmalinites; Bohemian Massif

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 19. 3. 2015 10:01, Mgr. Renata Čopjaková, Ph.D.

Anotace

V originále

Yttrium+REE contents in stratiform tourmalinites and their tourmaline from two different geological units, Svratka Unit and Krkonose-Jizera Unit (Bohemian Massif, Czech Republic) are reported to reveal tourmalinite genesis and tourmaline growth history. Premetamorphic tourmaline grains rimmed by younger metamorphic schorl-dravite were distinguished in both regions. The wing-shaped Y+REE patterns with minimum close to Eu in premetamorphic oxy-dravite from the Krkonose-Jizera Unit, and the Y+REE whole rock signature indicate important contribution of seawater in the oxy-dravite forming fluids. On the contrary, Y+REE patterns in premetamorphic schorl cores from the Svratka Unit correspond well to presumable exhalative origin of B-bearing fluids. Metamorphic rims of schorl-dravite at both regions show typically LREE-enriched patterns with pronounced positive Eu anomalies reflecting composition of metamorphic fluids.

Návaznosti

ED1.1.00/02.0068, projekt VaV

Název: CEITEC - central european institute of technology

GAP210/10/0743, projekt VaV

Název: Chemické složení a stupeň strukturního uspořádání přírodních turmalínů - geochemické versus strukturní faktory

Investor: Grantová agentura ČR, Chemické složení a stupeň strukturního uspořádání přírodních turmalínů - geochemické versus strukturní faktory

Citovat

ČOPJAKOVÁ, Renata, Radek ŠKODA, Milan NOVÁK a Michaela VAŠINOVÁ GALIOVÁ. Geochemistry of Y plus REE in stratiform tourmalinites and their tourmalines: implications for their genesis. In Jonsson, E. MINERAL DEPOSIT RESEARCH FOR A HIGH-TECH WORLD, VOLS. 1-4. UPPSALA: SGU-SVERIGES GEOLOGISKA UNDERSOKNING-GEOLOGY SURVEY SWEDEN, 2013, s. 1705-1708. ISBN 978-91-7403-207-9.

@inproceedings{1164699,
   author = {Čopjaková, Renata and Škoda, Radek and Novák, Milan and Vašinová Galiová, Michaela},
   address = {UPPSALA},
   booktitle = {MINERAL DEPOSIT RESEARCH FOR A HIGH-TECH WORLD, VOLS. 1-4},
   editor = {Jonsson, E},
   keywords = {Y plus REE; tourmaline; stratiform tourmalinites; Bohemian Massif},
   howpublished = {tištěná verze "print"},
   language = {eng},
   location = {UPPSALA},
   isbn = {978-91-7403-207-9},
   pages = {1705-1708},
   publisher = {SGU-SVERIGES GEOLOGISKA UNDERSOKNING-GEOLOGY SURVEY SWEDEN},
   title = {Geochemistry of Y plus REE in stratiform tourmalinites and their tourmalines: implications for their genesis},
   year = {2013}
}

TY  - JOUR
ID  - 1164699
AU  - Čopjaková, Renata - Škoda, Radek - Novák, Milan - Vašinová Galiová, Michaela
PY  - 2013
TI  - Geochemistry of Y plus REE in stratiform tourmalinites and their tourmalines: implications for their genesis
PB  - SGU-SVERIGES GEOLOGISKA UNDERSOKNING-GEOLOGY SURVEY SWEDEN
CY  - UPPSALA
SN  - 9789174032079
KW  - Y plus REE
KW  - tourmaline
KW  - stratiform tourmalinites
KW  - Bohemian Massif
N2  - Yttrium+REE contents in stratiform tourmalinites and their tourmaline from two different geological units, Svratka Unit and Krkonose-Jizera Unit (Bohemian Massif, Czech Republic) are reported to reveal tourmalinite genesis and tourmaline growth history. Premetamorphic tourmaline grains rimmed by younger metamorphic schorl-dravite were distinguished in both regions. The wing-shaped Y+REE patterns with minimum close to Eu in premetamorphic oxy-dravite from the Krkonose-Jizera Unit, and the Y+REE whole rock signature indicate important contribution of seawater in the oxy-dravite forming fluids. On the contrary, Y+REE patterns in premetamorphic schorl cores from the Svratka Unit correspond well to presumable exhalative origin of B-bearing fluids. Metamorphic rims of schorl-dravite at both regions show typically LREE-enriched patterns with pronounced positive Eu anomalies reflecting composition of metamorphic fluids.
ER  -

ČOPJAKOVÁ, Renata, Radek ŠKODA, Milan NOVÁK a Michaela VAŠINOVÁ GALIOVÁ. Geochemistry of Y plus REE in stratiform tourmalinites and their tourmalines: implications for their genesis. In Jonsson, E. \textit{MINERAL DEPOSIT RESEARCH FOR A HIGH-TECH WORLD, VOLS. 1-4}. UPPSALA: SGU-SVERIGES GEOLOGISKA UNDERSOKNING-GEOLOGY SURVEY SWEDEN, 2013, s.~1705-1708. ISBN~978-91-7403-207-9.

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