About Planet Green Metals:
Planet Green Metals is strategically building a premier Canadian critical mineral assets company, leveraging its expertise to acquire high-quality, de-risked mineral exploration and royalty properties. The Company currently holds six exploration properties in northern Ontario, covering copper, gold, VMS related base metals and lithium. Planet Green is actively pursuing the acquisition of promising new projects in Canada and North America to bolster the project portfolio and provide shareholders with a diversified commodity base that is resilient to price fluctuations and market forces. With a robust and fully integrated technical and corporate team, the Company is dedicated to maximizing shareholder value through new mineral discoveries in mining-friendly jurisdictions.
https://planetgreenmetals.com/sheraton-property/
SHERATON PROPERTY
The Sheraton Property is located 25 km southwest from Matheson, Ontario and 40 km eastsoutheast of Timmins, with excellent access via a network of forestry roads. The Sheraton Property consists of 102 claims located in the Province of Ontario, spanning across ~3,091 Hectares of terrain.
The property covers the geological contact of a sequence of felsic to intermediate volcanic and volcaniclastic rocks of the Wawa-Abitibi greenstone belt, which is highly prospective for Cu-ZnĀ±AuĀ±Ag VMS-style mineralization.
OVERVIEW
REGIONAL GEOLOGY & PAST EXPLORATION
Exploration by Cross Lake Minerals in the late 1990s on the adjacent property at Cross Lake identified bedded sulphides containing Zinc grades ranging from 1% to 6%, with local high-grade pods containing up to 18% Zn over a true width of 3 m, with silver values ranging up to 911 g/t Ag. Also, Copper grades of 1% to 3% were encountered over estimated true widths of up to 12 m (Vaillancourt, 2001).
The mineralization represents VMS style, and Planet Green will look for similar critical and precious metal mineralization on the Sheraton Property. The presence of significant copper mineralization at the adjacent Cross Lake property makes the Sheraton Property a compelling target.
https://planetgreenmetals.com/marion-property/
MARION PROPERTY
The Marion property is located 175 km north-northwest from Sudbury, and 100 km southwest of Timmins and consists of 53 claims located in the Province of Ontario.
Geologically the Marion Property contains a number of lithological and structural features that makes it a compelling target for gold exploration.
The historic trenching of the property identified 12.75 g/t Au over 9.15 m, and 135 m along strike the structure contained 2.18 g/t Au over 9.75 m (Domego Resources Ltd, 1979).
https://planetgreenmetals.com/rich-lake-property/
RICH LAKE
The Rich Lake property is located 365 km north-northeast from Thunder Bay and 17 km west of Fort Hope, Ontario and consists of 100 claims in the Province of Ontario.
The two claim blocks straddle along strike Separation Rapids Limitedās lithium, tantalum, cesium pegmatite Lilypad Project, where exploration identified several wide mineralized pegmatite dykes.
https://planetgreenmetals.com/grenfell-property/
GRENFELL PROPERTY
The Grenfell Property is located 13Ā kmĀ west-southwestĀ from Kirkland Lake,Ā Ontario, and has year-round access via Highway 11 and the Trans-Canada Highway
The Grenfell Property consists of four claims located in the Province of Ontario.
https://planetgreenmetals.com/harrison-road-lithium/
HARRISON ROAD LITHIUM PROPERTY
The Harrison Road Project consists of 38 mining claims comprising 6,080 hectares and is located 90 km northeast of Sioux Lookout, Ontario with easy highway and logging road access and good outcrop exposure.
The Project occurs within 6 km of a sub-province terrane boundary, an integral relationship between lithium deposits and structure. Lithium-bearing or LCT-pegmatites can occur up to 10 km away from their parental granite.
HISTORICAL MAPPING & EXPLORATION HISTORY
Planet Green Metals has conducted a heliborne magnetic survey and a sampling program, with plans for an extensive LiDAR survey and follow-up program in 2024.
Mapping by OGS in 1980 noted numerous tourmaline occurrences in the metasediments proximal to muscovite-bearing granites within the area.
āIn most cases the presence of abundant tourmaline in metasedimentary and metavolcanic rocks indicates the close proximity of a pegmatiteā.Ā ā (Beusetal., 1968, Cerny 1989) Observations from the 1990s and earlier have noted tourmaline occurrences indicative of pegmatite proximity, reinforcing the lithium prospectively of the area.
Preliminary surveys have shown elevated lithium levels in lake sediment samples within the property, higher than those around the known Root-McCombe pegmatite field.
https://planetgreenmetals.com/jeannette-lithium-exploration/
JEANNETTE LITHIUM
The Jeannette Lithium Project is situated approximately 84 km northeast of the town of Ear Falls and 105 km east of the mining community of Red Lake, Ontario. Spanning across 1,820 hectares, this property encompasses 4 claims that hold immense potential for the discovery of spodumene bearing pegmatites.
HISTORICAL WORK
During the 2022 field program 113 grab and channel samples were collected returning values up to 244 ppm Li, which was obtained from a sample of biotite gneiss with coarse feldspar-quartz dykelets. 45 grab samples were collected during the June and July field programs, which returned values up to 290 ppm Li and 688 ppm Rb. The value of 290 ppm Li was obtained from biotite gneiss proximal to the sample which had earlier returned 244 ppm Li. The value of 688 ppm Rb was obtained from pegmatite on the south shore of Tarpley Lake in the northeastern part of the Project
An additional 44 grab samples were collected during the August 2023 program. These returned up to 309 ppm Li and up to 497 ppm Rb. The value of 309 ppm Li was obtained from biotite gneiss proximal to samples which had earlier returned 244 and 290 ppm Li. The value of 497 ppm Rb was obtained from pegmatite approximately 2 km south of Tarpley Lake in the eastern part of the Project.
REGIONAL & PROJECT GEOLOGY
The Jeannette project is host to the Allison Lake batholith fractionation corridor and rare earth element enrichment as determined by elemental analysis and mineral observation in outcrop by Breaks et al., 2003. The SJ Pegmatite on the shore of Jubilee Lake is evidence that the Allison Lake batholith has produced external pegmatite dykes. Ā The Allison Lake East project is located in northwestern Ontario where numerous lithium deposits have been delineated to host significant reserves of Li2O.Ā Of significance is that the Li-deposits/projects of northwestern Ontario are located within 10-20 km of a terrane boundary. These terrane boundaries are deep seated sutures that divide accreted Archean terranes and act as conduits for fertile peraluminous granites. The Project is 20 km north of the English River-Uchi Terrane boundary.