Lithium One Metals Inc. Completes Remote Sensing; Accelerates Exploration At Sirmac East Lithium Project
as a major lithium district, boasting ten advanced stage projects and numerous early-stage occurrences. Notably, the Whabouchi Mine represents one of the world's largest bulk tonnage lithium deposits, with a Mineral Resource of 36.6 Mt at 1.3% Li2O, and an estimated mine life of 33 years.3 Additionally, the recently approved James Bay Lithium Mine has a Mineral Resource of 40.3 Mt at 1.4% Li2O and is proposed to produce an annual average of 321 Kt of spodumene concentrate over a 19-year mine life. Prospective Geology for Lithium Exploration. Spanning 656 ha, the Sirmac East Lithium Project is located in the northeastern part of the Superior geological province,
within the Frotet-Evans volcano-sedimentary belt. The project area features four lithologies: quartz-biotite-hornblende schists, amphibolitized flows and mafic sills, spodumene-bearing pegmatites and a syenite pluton measuring approximately 6 km in diameter. Both the Sirmac East Lithium Project and the Moblan Lithium deposit share a similar geological setting within the Frotet-Evans belt. The area is highly prospective for lithium hosted in spodumene-bearing pegmatites, with elevated historic lithium results in rocks reported on the property. The claims are contiguous with those of Vision Lithium, Winsome Resources and Troilus Gold. The Sirmac East Lithium Project is located in the northeastern part of the Superior geological province, in the Frotet-Evans volcano-sedimentary belt. Four lithologies are present in the project area: quartz-biotite-hornblende schists, amphibolitized flows or mafic sills, spodumene-bearing pegmatites and a syenite pluton measuring approximately 6 km in diameter. The structural trend is roughly east-west. Notable lithium deposits in the Frotet-Evans belt include Vision Lithium's Sirmac deposit (192 Kt of measured resources at 1.38% Li2O) and Sayona Mining's Moblan Lithium deposit (12.03 Mt at 1.4% Li2O mineral resource). Lithium mineralization in the region is associated with granitic, rare element-bearing spodumene-pegmatites.