Ville Marie
VILLE MARIE PROPERTY
Industrial Minerals Temiscaming property with unique geology also prospective for naturally occurring hydrogen and hellium
The Temiscamingue graben area is severely affected by seismicity and normal faulting related to extensional processes still active today (Fig. below). Such structures may be important in allowing the transfer of gases from deep sources to shallow environments. For H2 and He exploration, these faults must be well located in space (Lidar, AMT, gravity, magnetometric surveys) and geophysical surveys must be carried out in order to verify the vertical extension (in depth) of the faults. The deeper these structures are, the greater the potential for gas transfer.
QI Materials Témiscamingue property offers similar geology to the recent large natural hydrogen Ramsey Project discovery by GoldHydrogen Ltd in South Australia.
“The conceptual exploration model that led to the development of the exploration program is the hydrogen production model in the context of Precambrian basement and more specifically the sub-model linked to the presence of iron-rich rocks associated Archean greenstone belt In the Témiscamingue area and more precisely in the St-Brunode-Guigues sector, the units of the Baby volcanic belt containing peridotites, komatiites, basalts and iron formation.”
Furthermore, “These sedimentary rocks, covering the Precambrian basement, are affected by the still active Temiscamingue rift zone (neotectonic deformations),” said Marc Richer-LaFlèche, of the INRS who is heading the program.