Abstract Details
(2020) In situ Measurements of Li Isotopes in Quartz: Implications for Magmatic-Hydrothermal Evolution of Koktokay No.3 Rare Metal Pegmatite
Gao Y-Y, Zhou Q-F & Qin K-Z
https://doi.org/10.46427/gold2020.793
08i: Plenary Hall, Friday 26th June 22:09 - 22:12
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Submitted by Bénédicte Cenki-Tok on Thursday 25th June 01:25
Thanks for this very interesting presentation. It seems that Li isotopes fractionation is linked to fractional crystallisation. Is there any way to use this technique to track the origin of fluids involved in pegmatite formation as well ?
Thanks for this very interesting presentation. It seems that Li isotopes fractionation is linked to fractional crystallisation. Is there any way to use this technique to track the origin of fluids involved in pegmatite formation as well ?
Submitted by Kathryn Goodenough on Friday 26th June 11:56
Many thanks for the presentation, this is really interesting. Did your CL work enable you to identify more than one generation of quartz in individual samples? And if so, could this be linked to different Li isotope populations?
Many thanks for the presentation, this is really interesting. Did your CL work enable you to identify more than one generation of quartz in individual samples? And if so, could this be linked to different Li isotope populations?
Submitted by Mona Sirbescu on Friday 26th June 20:02
Very nice results! Fluid inclusions are very abundant in pegmatite quartz and can have high Li contents, orders of magnitude higher than quartz. I am wondering how do you prevent contamination from fluid inclusions during SIMS analysis?
Very nice results! Fluid inclusions are very abundant in pegmatite quartz and can have high Li contents, orders of magnitude higher than quartz. I am wondering how do you prevent contamination from fluid inclusions during SIMS analysis?
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