Max Resource Discovers 5 New Copper and Silver Targets at CESAR

In This Article:

Vancouver, British Columbia--(Newsfile Corp. - February 7, 2024) - MAX RESOURCE CORP. (TSXV: MAX) (OTC Pink: MXROF) (FSE: M1D2) ("Max" or the "Company") is pleased to report that it has discovered a series of five mineralized outcrops (collectively Target Area AM-14) on a Mining Concession, within the AM District of its wholly-owned Cesar Copper-Silver Project, Northeastern Colombia.

Highlights

  • 5 newly discovered outcrops of stratiform copper-silver mineralization covering 1,000m2.

  • Mineralized layers are exposed up to 285m along strike and range in thickness from 0.8m to 4.0m.

  • Confirms multiple copper-silver bearing horizons within thick sedimentary rock sequence.

  • Strong evidence of 1.5-km continuity of mineralized layers between new discovery and AM-07.

The five discoveries confirm multiple copper-silver bearing layers within a 700-metre-thick sequence of interbedded sandstones in the AM District. Additionally, there is strong evidence to suggest that one of the newly discovered outcrops (Outcrop #2) is a continuation of the mineralized horizon at target AM-07, located approximately 1.5-km to the northeast. This supports the Company's interpretation that the copper-silver bearing layers in the AM District are continuous over large distances, similar to the Kupferschiefer and Kamoa-Kakula deposits.

"As we continue to obtain high-grade results and locate significant structural and stratiform copper-silver mineralization, the Company's staunch belief in Cesar as a potential for significant deposits comes ever closer to fruition," commented Brett Matich, CEO of Max.

"The AM-14 mapping and sampling outlines an area some 600 to 1000 metres by 1000 to 1200 metres, strongly supporting our belief in Cesar as a regional or district copper-silver target, as opposed to a cluster of smaller unrelated zones. We look forward to assay results in the coming weeks," he concluded.

Description of the Mineralisation
Preliminary work has determined that mineralization is hosted in layers of medium to fine-grained sandstone rich in organic material. The copper-silver bearing horizons are distributed across a 700-metre-thick package of interbedded sedimentary rocks that strike 240? to 260? and dip 30? to 45? northwest. Chalcocite, malachite and azurite are the most abundant copper minerals observed in the outcrop (refer to Figure 1 to Figure 3).

All five of the outcropping mineralized beds are open along strike and at Outcrop #2, the copper-silver bearing sandstone horizon could be traced along strike for over a distance of 285m. Similarly, at Outcrop #5, the mineralized horizon exposed for over 130m before disappearing under cover. Layer thickness ranges from 0.8m at Outcrop #4 to 4.0m at Outcrop #5.