Fabled Reports on Geological / Structural Survey on the Bronson Copper Property

VANCOUVER, BC / ACCESSWIRE / June 29, 2022 / Fabled Copper Corp. ("Fabled Copper" or the "Company") (CSE:FABL; FSE:XZ7) announces additional results of 2021 surface field work on its Muskwa Copper Project. See Figure 1 below.

Figure 1 - General Property Location

Foto: Accesswire

The Muskwa Project is comprised of the Neil, the Toro and the Bronson Properties in northern British Columbia. See Figure 2 below.

Figure 2 - Location Map

Foto: Accesswire

Peter Hawley, President, CEO reports; "We have started reporting on the Bronson property with the various surveys conducted on the Book 6 copper occurrence and now the bigger picture, the geology and structural interpretation of the entire Bronson property." See Figure 3 below.

Figure 3 - Bronson Property Location

Foto: Accesswire

Bronson Property Geology / Structure

Three main stratigraphic units underlie the Bronson property including the Paleoproterozoic Aida and Gataga Formations and the Ordivician Kechika Group. Diabase units intrude both the Aida and Gataga Formations but were not observed in the Kechika Group.

The Aida Formation consists of interbedded dolostone, limestone, shale, and sandstone. The Gataga Formation consists of dark grey too live grey pyritic, non-calcareous shales with subordinate sandstone and siltstone.

The Kechika Group occurs which occurs as a small window in the northeastern corner of the claim block, consists of massive limestone and calcareous quartz sandstone.

The stratigraphy is broadly NNW trending and moderately to gently dipping SW throughout the property. No macroscale folding is observed from satellite imagery or in historical geological map interpretations. Younger thrust faulting of the Aida formation over the Gataga Formation occurs in the SE portion of the property. Additionally, the Gataga thrust is interpreted to occur between the Aida Formation and the Kechika Group in the northeastern corner of the Bronson property.

Three main orientations of lineaments and later brittle faults are also observed across the property including first-order N-NNW lineaments and second-order ubiquitous NE and less well-developed NW lineaments.

These are suggested to represent kinematically-related fault sets that are associated with Cu-Co mineralization present across the Bronson Property. See Figure 4 below.

Figure 4 - Bronson Property Integrated Geological Interpretation