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Project: | PAK | |
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Deposit: | Spark | |
Location: | Canada | |
Commodities: | Lithium-Tantalum-Caesium-Rubidium | |
Date: | 9/25/2019 | |
Report Code: | NI43-101 | |
Report Type: | Exploration/Drilling Update | |
Project Stage: | Pursuing Feasibility Study | |
Report details: | 25-9-2019: Frontier Lithium Inc. announces an Exploration/Drilling Update report for its Spark deposit at the PAK project. Drilling results incl. 231.05m @ 1.61% Li2O from 55m. SUDBURY, ON, Sept. 24, 2019 /CNW/ - Frontier Lithium Inc. (TSX.V: FL) (the "Co | |
Resources: | (Resource): 9.3Mt @ 2.04% Li2O | |
CP/QP: | [Overall Report]: Garth Drever (Internal) | |
ABSTRACT: | SUDBURY, ON, Sept. 24, 2019 /CNW/ - Frontier Lithium Inc. (TSX.V: FL) (the "Company) is pleased to announce the initial results of their second Phase of drilling on the Spark Pegmatite. Frontier completed four diamond drill holes totaling 1,159.5 m in July-August 2019. During the drill program an additional 4 channels totaling 52 m were cut and most of the exposed outcrop surface in the immediate area of the pegmatite was mapped. Geochemical results from the first two drill holes have been received. The remaining analysis is expected by the end of October. Figure 1 is a location map showing the surface outline of the Spark pegmatite, location of channels and drill hole traces with geology overlain on detailed imagery of the outcrop area. Phase I drilling in February focused on targeting the pegmatite from the south along the base of the 30 to 40 m high ridge of predominately pegmatite. Three holes were drilled during Phase II from the top of the ridge back towards the Phase I collars and the fourth hole was a re-drill of hole PL-037-19 which had been abandoned. All holes intersected significant widths from 20 to 125 m of pegmatite. Spodumene grain size and abundance tends to increase with the presence of quartz and feldspar megacrysts which is similar to the LIZ (Lower Intermediate Zone) and locally similar to the CIZ (Central Intermediate Zone) of the PAK Pegmatite. The exposed pegmatite and host metavolcanic rock has been mapped over most of the immediate area (Figures 1). Overburden stripping is required to the west and to the east in the area of Channels 39 and 40. | |
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