1. Reactivation mechanisms and related-porosity enhancement of shear zones in the context of basement-hosted uranium mineralization: case of the Spitfire discovery in the Patterson Lake corridor, Canada
2. Thermotectonic events recorded by U-Pb geochronology and Zr-in-rutile thermometry of Ti oxides in basement rocks along the P2 fault, eastern Athabasca Basin, Saskatchewan, Canada;Adlakha E.;GSA Bulletin,2021
3. Alteration within the basement rocks associated with the P2 fault and the McArthur River uranium deposit, Athabasca Basin;Adlakha E.E.;Geological Survey of Canada, Open File Report,2013
4. Adlakha, E.E., Hatori, K., Zaluski, G., Kotzer, T.G., Davis, W.J. and Potter, E.G. 2015. Mineralogy of a fertile fluid conduit related to unconformity-type uranium depositys in the Athabasca Basin, Saskatchewan. In: Potter, E.G. and Wright, D.M. (eds) Targeted Geoscience Initiative 4: Unconformity-Related Uranium Systems. Geological Survey of Canada, Open File 7791, 74–82, https://doi.org/10.4095/295776
5. The origin of Ti-oxide minerals below and within the eastern Athabasca Basin, Canada