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Statements

Subject Item
n2:RIV%2F61989592%3A15310%2F11%3A33118757%21RIV12-MSM-15310___
rdf:type
n16:Vysledek skos:Concept
dcterms:description
Tourmalines (dravite - schorl - uvite - povondraite) from intragranitic pegmatites of the Třebíč Pluton (porphyritic,amphibole-biotite melasyenite to quartz melasyenite - melagranite), in the Czech Republic, were examined using an electron microprobe, Mössbauer spectroscopy and LA-ICP-MS analyses. Pegmatites with the common assemblage Kfs + qtz + pl (An0-13) + Fe-rich phlogopite (0.49 { XMg { 0.70) and accessory allanite-(Ce), ilmenite, tourmaline and titanite, were divided into three types generally related to the NYF (REL-REE) pegmatites: allanite-type, euxenite-type (+ euxenite, aeschynite, pyrochlore, beryl, niobian rutile, zircon), and the most evolved euxenite-type pegmatite, Klučov I (with annite, XMg 0.09), cassiterite, herzenbergite, and abundant graphic intergrowths of quartz + feldspars and quartz + tourmaline). Black tourmaline occurs in several distinct morphological, paragenetic and textural types with very high variability in zoning; however, the morphological types of tourmaline do not differ chemically. Tourmalines (dravite - schorl - uvite - povondraite) from intragranitic pegmatites of the Třebíč Pluton (porphyritic,amphibole-biotite melasyenite to quartz melasyenite - melagranite), in the Czech Republic, were examined using an electron microprobe, Mössbauer spectroscopy and LA-ICP-MS analyses. Pegmatites with the common assemblage Kfs + qtz + pl (An0-13) + Fe-rich phlogopite (0.49 { XMg { 0.70) and accessory allanite-(Ce), ilmenite, tourmaline and titanite, were divided into three types generally related to the NYF (REL-REE) pegmatites: allanite-type, euxenite-type (+ euxenite, aeschynite, pyrochlore, beryl, niobian rutile, zircon), and the most evolved euxenite-type pegmatite, Klučov I (with annite, XMg 0.09), cassiterite, herzenbergite, and abundant graphic intergrowths of quartz + feldspars and quartz + tourmaline). Black tourmaline occurs in several distinct morphological, paragenetic and textural types with very high variability in zoning; however, the morphological types of tourmaline do not differ chemically.
dcterms:title
Compositional Trends in Tourmaline from Intragranitic NYF Pegmatites of the Třebíč Pluton, Czech Republic: An Electron Microprobe, Mössbauer and LA-ICP-MS Study Compositional Trends in Tourmaline from Intragranitic NYF Pegmatites of the Třebíč Pluton, Czech Republic: An Electron Microprobe, Mössbauer and LA-ICP-MS Study
skos:prefLabel
Compositional Trends in Tourmaline from Intragranitic NYF Pegmatites of the Třebíč Pluton, Czech Republic: An Electron Microprobe, Mössbauer and LA-ICP-MS Study Compositional Trends in Tourmaline from Intragranitic NYF Pegmatites of the Třebíč Pluton, Czech Republic: An Electron Microprobe, Mössbauer and LA-ICP-MS Study
skos:notation
RIV/61989592:15310/11:33118757!RIV12-MSM-15310___
n16:predkladatel
n21:orjk%3A15310
n3:aktivita
n10:Z n10:P
n3:aktivity
P(ED2.1.00/03.0058), P(GAP210/10/0743), Z(MSM6198959218)
n3:cisloPeriodika
1
n3:dodaniDat
n11:2012
n3:domaciTvurceVysledku
n4:5207193
n3:druhVysledku
n15:J
n3:duvernostUdaju
n8:S
n3:entitaPredkladatele
n6:predkladatel
n3:idSjednocenehoVysledku
191460
n3:idVysledku
RIV/61989592:15310/11:33118757
n3:jazykVysledku
n14:eng
n3:klicovaSlova
tourmaline, dravite - schorl - uvite - povondraite, electron microprobe, Mössbauer spectroscopy, LA-ICP-MS, compositional trends, substitution mechanisms, NYF pegmatites, Třebíč Pluton, Czech Republic.
n3:klicoveSlovo
n7:substitution%20mechanisms n7:dravite n7:Czech%20Republic. n7:compositional%20trends n7:NYF%20pegmatites n7:M%C3%B6ssbauer%20spectroscopy n7:T%C5%99eb%C3%AD%C4%8D%20Pluton n7:tourmaline n7:electron%20microprobe n7:LA-ICP-MS
n3:kodStatuVydavatele
CA - Kanada
n3:kontrolniKodProRIV
[4D3FD67ED4A7]
n3:nazevZdroje
Canadian Mineralogist
n3:obor
n19:DB
n3:pocetDomacichTvurcuVysledku
1
n3:pocetTvurcuVysledku
5
n3:projekt
n20:ED2.1.00%2F03.0058 n20:GAP210%2F10%2F0743
n3:rokUplatneniVysledku
n11:2011
n3:svazekPeriodika
49
n3:tvurceVysledku
Novák, Milan Škoda, Radek Filip, Jan Vaculovič, Tomáš Macek, Ivo
n3:wos
000288240400023
n3:zamer
n18:MSM6198959218
s:issn
0008-4476
s:numberOfPages
22
n12:doi
10.3749/canmin.49.1.359
n17:organizacniJednotka
15310