Express Lithium Project
Québec, Canada
To the north, the trend of pegmatite intrusions at the James Bay deposit are generally WNW to ESE. To the south, the bedrock and pegmatite intrusions within the Chambois Greenstone Belt are generally SW to NE. The two trends appear to converge circa the Express Lithium Project. Geophysical data and satellite data is to be acquired to identify the key target areas for the sampling program. In -country geological partners, Dahrouge Geological, are overseeing exploration programs.
The main claim block is underlain by muscovite and tourmaline bearing pegmatite with enclaves of pegmatite, while the smaller claim block is underlain by the Chambois Greenstone Belt. Outcropping pegmatites are evident from satellite imagery, and high-priority pegmatites have been identified along trend from government mapping. It has been termed ‘The Spodumene Suite’ by Quebec’s MERN, yet this ground has never been explored for lithium.
The main claim block is underlain by muscovite and tourmaline bearing pegmatite with enclaves of pegmatite, while the smaller claim block is underlain by the Chambois Greenstone Belt. Outcropping pegmatites are evident from satellite imagery, and high-priority pegmatites have been identified along trend from government mapping. It has been termed ‘The Spodumene Suite’ by Quebec’s MERN, yet this ground has never been explored for lithium.
To the north, the trend of pegmatite intrusions at the James Bay deposit are generally WNW to ESE. To the south, the bedrock and pegmatite intrusions within the Chambois Greenstone Belt are generally SW to NE. The two trends appear to converge circa the Express Lithium Project. Geophysical data and satellite data is to be acquired to identify the key target areas for the sampling program. In -country geological partners, Dahrouge Geological, are overseeing exploration programs.
