RE:Completion of N143-101 for 100% Owned Buckingham ProjectSee detailed technical results here!
https://gratomic.ca/wp-content/uploads/2020/12/20201209-Buckingham-2018-Technical-Report-Final.pdf28.pdf
The Buckingham graphite property of Gratomic Inc. hosts significant graphite and includes both vein and disseminated styles of mineralization. The mineralization occurs in two main zones: the Uncle Zone and the Case Zone. Disseminated flake type graphite is the more widespread style of mineralization and occurs throughout the paragneiss and marble sequence comprising the Case Zone. The vein type graphite occurs as cm scale veins of coarse-grained graphite typically hosted in marble and/or paragneiss of the Uncle Zone. Graphite occurs at surface in both zones.