Neptune Property

Overview

The Neptune Property is a lithium-focused exploration project located in the Eeyou Istchee James Bay region of Northern Québec. The project spans 6,897 hectares across 129 mineral claims, positioned approximately 3 km east of the Billy Diamond Highway and 65 km south of Camp 509. The area is gaining recognition for its potential to host lithium–cesium–tantalum (LCT) pegmatites.

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Location & Accessibility

The Neptune Property is a lithium-focused exploration project located in the Eeyou Istchee James Bay region of Northern Québec. The project spans 6,897 hectares across 129 mineral claims, positioned approximately 3 km east of the Billy Diamond Highway and 65 km south of Camp 509. The area is gaining recognition for its potential to host lithium–cesium–tantalum (LCT) pegmatites.

Geology

The Neptune Property is underlain by tonalite, granodiorite, quartz diorite, and metasedimentary rock units, within the La Grande Sub-province—a region that hosts several active lithium exploration projects. These rock types are considered favorable for LCT pegmatite intrusion.

Historical Exploration

Exploration prior to 2024 was limited. However, the property was staked based on notable government lake sediment anomalies in lithium, cesium, and rubidium, which are pathfinder elements for LCT pegmatites. The regional geological context also supports the property’s potential.

2024 Field Program

The exploration campaign conducted in 2024 included:

  • High-resolution LiDAR and satellite imagery

  • A 785 line-kilometre heliborne magnetic survey

  • Ground-based prospecting, mapping, and geochemical sampling

Crews identified several pegmatite outcrops, some with coarse feldspar and quartz, along with accessory muscovite, garnet, and biotite—minerals commonly associated with evolved pegmatite systems.

Geochemical Results

A total of 51 rock samples were collected. Highlights include:

  • Highest lithium value: 84 ppm Li (0.0181% Li₂O)

  • Tantalum: Up to 70.6 ppm Ta

  • Niobium: Up to 552 ppm Nb

Multiple samples exhibited K/Rb <150 and Nb/Ta <8, suggesting the presence of geochemically evolved pegmatites—key indicators of LCT potential.

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Exploration Potential

While spodumene was not observed during the 2024 program, the identification of fertile geochemical markers and the presence of widespread pegmatite dykes indicate strong potential for lithium mineralization. Several areas across the central and southeastern portions of the property remain underexplored and are recommended for follow-up.

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