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Statements

Subject Item
n2:RIV%2F00216305%3A26110%2F11%3APU97320%21RIV12-MSM-26110___
rdf:type
n15:Vysledek skos:Concept
dcterms:description
The western part of the Khan Bogd complex, located in South Gobi (southern Mongolia), comprises (in order of emplacement): microcline-phyric granite, peralkaline aegirine-arfvedsonite granite (main intrusive phase) and aplite-pegmatite veins confined predominantly to the apical parts of the intrusion. These rocks are interpreted to represent products of extreme fractional crystallization involving alkali feldspar, quartz and, to a lesser extent, ferromagnesian silicates and, in the final stages of magma evolution, release of a silica-saturated orthomagmatic fluid. Geochemically, this evolutionary path involved an increase in index of peralkalinity (from 1.0 in the porphyritic granite to 1.3 in the main phase to 2.5 in the pegmatite) and whole-rock Zr content (864 to 1130 to 16900 ppm). In the porphyritic granite, zircon with a low Hf content (Zr/Hf = 55-75) is the principal Zr phase, whereas alkali-Ca zirconosilicate minerals are characteristically absent. Zirconium mineralogy in the peralkaline grani The western part of the Khan Bogd complex, located in South Gobi (southern Mongolia), comprises (in order of emplacement): microcline-phyric granite, peralkaline aegirine-arfvedsonite granite (main intrusive phase) and aplite-pegmatite veins confined predominantly to the apical parts of the intrusion. These rocks are interpreted to represent products of extreme fractional crystallization involving alkali feldspar, quartz and, to a lesser extent, ferromagnesian silicates and, in the final stages of magma evolution, release of a silica-saturated orthomagmatic fluid. Geochemically, this evolutionary path involved an increase in index of peralkalinity (from 1.0 in the porphyritic granite to 1.3 in the main phase to 2.5 in the pegmatite) and whole-rock Zr content (864 to 1130 to 16900 ppm). In the porphyritic granite, zircon with a low Hf content (Zr/Hf = 55-75) is the principal Zr phase, whereas alkali-Ca zirconosilicate minerals are characteristically absent. Zirconium mineralogy in the peralkaline grani
dcterms:title
Distribution and evolution of zirconium mineralization in peralkaline granites and associated pegmatites of the Khan Bogd complex, southern Mongolia Distribution and evolution of zirconium mineralization in peralkaline granites and associated pegmatites of the Khan Bogd complex, southern Mongolia
skos:prefLabel
Distribution and evolution of zirconium mineralization in peralkaline granites and associated pegmatites of the Khan Bogd complex, southern Mongolia Distribution and evolution of zirconium mineralization in peralkaline granites and associated pegmatites of the Khan Bogd complex, southern Mongolia
skos:notation
RIV/00216305:26110/11:PU97320!RIV12-MSM-26110___
n15:predkladatel
n16:orjk%3A26110
n3:aktivita
n11:I n11:Z
n3:aktivity
I, Z(MSM0021622412), Z(MSM6215648902)
n3:cisloPeriodika
4
n3:dodaniDat
n9:2012
n3:domaciTvurceVysledku
n5:8694583
n3:druhVysledku
n14:J
n3:duvernostUdaju
n18:S
n3:entitaPredkladatele
n7:predkladatel
n3:idSjednocenehoVysledku
194941
n3:idVysledku
RIV/00216305:26110/11:PU97320
n3:jazykVysledku
n10:eng
n3:klicovaSlova
gittinsite, Mongolia, zircon, Gobi desert, elpidite, granitic pegmatite, peralkaline granite, Khan Bogd, Zr mineralization, armstrongite
n3:klicoveSlovo
n4:Gobi%20desert n4:Zr%20mineralization n4:Mongolia n4:elpidite n4:granitic%20pegmatite n4:Khan%20Bogd n4:peralkaline%20granite n4:gittinsite n4:armstrongite n4:zircon
n3:kodStatuVydavatele
CA - Kanada
n3:kontrolniKodProRIV
[CC4BD882130C]
n3:nazevZdroje
CANADIAN MINERALOGIST
n3:obor
n12:DB
n3:pocetDomacichTvurcuVysledku
1
n3:pocetTvurcuVysledku
5
n3:rokUplatneniVysledku
n9:2011
n3:svazekPeriodika
49
n3:tvurceVysledku
Krmíček, Lukáš
n3:zamer
n8:MSM6215648902 n8:MSM0021622412
s:issn
0008-4476
s:numberOfPages
19
n19:organizacniJednotka
26110