Technical Report and Recommendations Summer 2017 Trieste Project, Québec Osisko Mining
Previous drilling cores and sampling may still be available in a shed somewhere to be re-assayed for lithium I hope. Mapping data of the Pegmatite dykes will certainly save time for field exploration work.
https://gq.mines.gouv.qc.ca/documents/examine/GM70437/GM70437.pdf
Pegmatite Pegmatite dyke occurrences were more abundant in the metasedimentary package on the property. Moreover, in the southern part of the NW grid, several outcrops of pegmatite rich in muscovite (5- 20%) were outlined near the contact between the volcanic rocks to the north and the metasedimentary rocks to the south. The other minerals contained in these pegmatites are quartz (25-35%) and plagioclase (50-60%), thus representing a tonalitic composition. The abundance in muscovite along the contact between volcanics and the metasedimentary unit should be kept in mind as a favourable conduct for fluids rich in water.
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