About: A unique Mo deposit associated with carbonatites in the Qinling orogenic belt, central China     Goto   Sponge   NotDistinct   Permalink

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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 (en)
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 (en)
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 (en)
skos:notation
  • RIV/62156489:43410/10:00155472!RIV11-MSM-43410___
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • Z(MSM6215648902)
http://linked.open...iv/cisloPeriodika
  • 1-2
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
http://linked.open.../riv/druhVysledku
http://linked.open...iv/duvernostUdaju
http://linked.open...titaPredkladatele
http://linked.open...dnocenehoVysledku
  • 245053
http://linked.open...ai/riv/idVysledku
  • RIV/62156489:43410/10:00155472
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • Huanglongpu; mantle source; REE minerals; carbonatite; Mo deposits; molybdenite (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • NL - Nizozemsko
http://linked.open...ontrolniKodProRIV
  • [B59F9CDE728C]
http://linked.open...i/riv/nazevZdroje
  • Lithos
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 118
http://linked.open...iv/tvurceVysledku
  • Kynický, Jindřich
  • Chakhmouradian, Anton
  • Cheng, Xu
  • Song, Wenlei
  • Qi, Liang
http://linked.open...n/vavai/riv/zamer
issn
  • 0024-4937
number of pages
http://localhost/t...ganizacniJednotka
  • 43410
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