Frontier Lithium Strikes High-Grade Lithium at Ember Pegmatite 1km from the Spark Resource

In This Article:

SUDBURY, ON, Nov. 19, 2024 /CNW/ - Frontier Lithium Inc. (TSXV: FL) (FRA: HL2) (OTCQX: LITOF) ("Frontier" or "the Company"), is pleased to announce progress on fieldwork activities supporting Phase 1 of the definitive feasibility study on the PAK Lithium Project and provide an exploration update, including details on the maiden drillhole at the Ember LCT pegmatite, located 1 km west-northwest of the Spark deposit.

Highlights

  • DDH PL-138-24 intersected 18.8 metres of pegmatite from 42.7 to 61.4 meters, averaging 1.43% Li2O.

  • Lithogeochemical orientation survey completed over the Spark deposit and surrounding area.

The Ember pegmatite originally called Spark-Ext, was channeled in 2023 with two parallel channels averaging 2.16% Li2O over the combined length of 18 m including 6m averaging 3.27% Li2O (Press Release Sept 25, 2023).

"Results from PL-138-24 have extended the high-grade lithium zone at surface to a depth of 40 metres, further enhancing the exploration potential of the pegmatite" states Garth Drever, VP Exploration "Structural measurements on the outcrop and from oriented drill core suggest a West Southwest-East Northeast orientation of the Ember pegmatite which is consistent to the Spark deposit suggesting a possible en echelon structural relationship. Since they share similar textural and mineralogical features, the unexposed potential of Ember could prove to be significant."

During the same period, three condemnation diamond drill holes were completed on proposed stockpile sites for definitive feasibility study and a small-scale regional exploration program was completed. Field mapping and prospecting on claim blocks north of the mining leases identified target areas that will require further work, including detailed mapping and channel sampling. A lithogeochemical orientation survey was initiated by sampling host rock at the Spark and Bolt pegmatites and surrounding areas, including the Ember pegmatite. The objective is to assess the potential of identifying unexposed pegmatites by vectoring towards areas of higher fractionation.

Figure 1 is a compilation map shows the location of the two channels and drill hole PL-138-24 at Ember in both plan and section view. The dashed lines on the lower right map outlines the potential extension of the Ember pegmatite which is also an area of glacial ground moraine with abundant glacial erratics (boulders) of varying size and composition. Further work is required to determine the thickness of the overlying glacial material away from the exposed portion of the pegmatite.