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Statements

Subject Item
n2:RIV%2F62156489%3A43410%2F10%3A00155472%21RIV11-MSM-43410___
rdf:type
n12:Vysledek skos:Concept
dcterms:description
The Qinling molybdenum belt is a prominent metallogenic structure in central China hosting several significant porphyry- and porphyry-skarn-type deposits. The Huanglongpu Mo deposit in the north-western part of the belt is unique in that it is associated with carbonatite dykes, rather than felsic magmatism. The carbonatites are composed largely of Sr-Mn-rich calcite and characterized by high concentrations of Sr and rare-earth elements (REE), and stable-isotope values indicative of a mantle source (delta13CPDB = -- 6.7 and delta18OSMOW = 8.2). Molybdenite is associated with galena and REE minerals (parisite, bastnäsite and monazite). Both molybdenite and galena are characterized by high Re contents (up to 0.4 and 0.2 wt.%, respectively) and Re/(Mo, Pb) ratios approaching the primitive-mantle values. In contrast to the rock-forming calcite, the REE minerals are enriched in light REE, whose relative proportion increases from parisite-(Ce) [average (La/Nd)n = 2.1] to bastnäsite-(Ce) and monazite-(Ce) [av The Qinling molybdenum belt is a prominent metallogenic structure in central China hosting several significant porphyry- and porphyry-skarn-type deposits. The Huanglongpu Mo deposit in the north-western part of the belt is unique in that it is associated with carbonatite dykes, rather than felsic magmatism. The carbonatites are composed largely of Sr-Mn-rich calcite and characterized by high concentrations of Sr and rare-earth elements (REE), and stable-isotope values indicative of a mantle source (delta13CPDB = -- 6.7 and delta18OSMOW = 8.2). Molybdenite is associated with galena and REE minerals (parisite, bastnäsite and monazite). Both molybdenite and galena are characterized by high Re contents (up to 0.4 and 0.2 wt.%, respectively) and Re/(Mo, Pb) ratios approaching the primitive-mantle values. In contrast to the rock-forming calcite, the REE minerals are enriched in light REE, whose relative proportion increases from parisite-(Ce) [average (La/Nd)n = 2.1] to bastnäsite-(Ce) and monazite-(Ce) [av
dcterms:title
A unique Mo deposit associated with carbonatites in the Qinling orogenic belt, central China A unique Mo deposit associated with carbonatites in the Qinling orogenic belt, central China
skos:prefLabel
A unique Mo deposit associated with carbonatites in the Qinling orogenic belt, central China A unique Mo deposit associated with carbonatites in the Qinling orogenic belt, central China
skos:notation
RIV/62156489:43410/10:00155472!RIV11-MSM-43410___
n3:aktivita
n18:Z
n3:aktivity
Z(MSM6215648902)
n3:cisloPeriodika
1-2
n3:dodaniDat
n9:2011
n3:domaciTvurceVysledku
n15:4733029
n3:druhVysledku
n7:J
n3:duvernostUdaju
n16:S
n3:entitaPredkladatele
n8:predkladatel
n3:idSjednocenehoVysledku
245053
n3:idVysledku
RIV/62156489:43410/10:00155472
n3:jazykVysledku
n6:eng
n3:klicovaSlova
Huanglongpu; mantle source; REE minerals; carbonatite; Mo deposits; molybdenite
n3:klicoveSlovo
n4:molybdenite n4:Mo%20deposits n4:mantle%20source n4:REE%20minerals n4:Huanglongpu n4:carbonatite
n3:kodStatuVydavatele
NL - Nizozemsko
n3:kontrolniKodProRIV
[B59F9CDE728C]
n3:nazevZdroje
Lithos
n3:obor
n17:DB
n3:pocetDomacichTvurcuVysledku
1
n3:pocetTvurcuVysledku
5
n3:rokUplatneniVysledku
n9:2010
n3:svazekPeriodika
118
n3:tvurceVysledku
Kynický, Jindřich Qi, Liang Cheng, Xu Song, Wenlei Chakhmouradian, Anton
n3:zamer
n14:MSM6215648902
s:issn
0024-4937
s:numberOfPages
11
n5:organizacniJednotka
43410