Feldspar and Quartz Crystals Unveil the Petrogenesis of the Lithium-rich Moblan Pegmatite (Quebec)
Previously Published Material: Experimental evidence for the supersaturation of pegmatite-forming melts in Li-aluminosilicates was presented in the GSA meeting in Vancouver in October 2014 and the GAC-MAC conference in Fredericton in May 2014. Part of the findings summarized in this abstract have been submitted for publication to the journal Contributions to Mineralogy and Petrology.
Abstract ID#: 36099
The Li concentration of the main minerals from different zones of the Moblan pegmatite is used in combination with experimental results in order to evaluate the Li enrichment of the granitic melt that generated the central sill. The Li concentration of the melt that coexisted with Li-rich feldspar and quartz crystals can reach up to ~7000 ppm, suggesting supersaturation of the pegmatite-forming melt in Li-aluminosilicate phases. In addition, the uncommon geochemical signature of Li in feldspar can be used as a useful exploration tool for the identification and targeting of Li-rich pegmatites.
