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Delta I-Zone Channel Samples Return 1.23 g/t Gold Over 40.6 metres and 2.4 g/t Gold Over 16.2 metres In a 5 metre Wide Dike at Surface at The Delta-1 Property in Thunder Bay, Ontario

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Kingston, Ontario--(Newsfile Corp. - December 17, 2024) - Delta Resources Limited (TSXV: DLTA) (OTC Pink: DTARF) (FSE: 6GO1) ("Delta" or "The Company") is pleased to announce that it has received and tabulated assay results from channel sampling of the I-Zone at the Delta-1 Expansion Property in Thunder Bay, Ontario.

Two parallel channel samples were taken in a 5-metre wide dike known as the "I-Zone", adjacent to channel samples taken by Inco Gold in 1988-89 for which results were left unreported. The channel samples tested the complete length of the exposed dike. Channels were cut perpendicularly to quartz-carbonate-pyrite veins and veinlets but parallel to the dike contacts (Figure 1). Results from the two channel samples are as follows:

  • CHANNEL #1: 1.23 g/t Au over 40.6 m incl. 2.12 g/t Au over 12 m and 3.39 g/t Au over 5 m

  • CHANNEL #2: 2.40 g/t Au over 16.2 m incl. 5.54 g/t Au over 5 m

Figure 1: Geological map of the I-Zone and location of the channel samples.

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Gold mineralization consists of 1-20 cm wide quartz-carbonate-pyrite extension veins and veinlets with visible gold, hosted by a granodiorite dike that is approximately 5 metres wide (Photo 1). Gold mineralization also occurs as millimetre-scale pyrite stringers and fracture-filling. The quartz veins trend NS and dip steeply towards the west while the dike is generally trending EW and dipping steeply towards the south. Veins and veinlets typically end abruptly at the contacts of the granodiorire dikes. At the I-Zone, the granodiorite dike is hosted by iron formations.

Red potassic, hematitic and pyritic alteration is intense and texture destructive, intensifying along the contacts of the veins and fractures (Photo 2). Host rocks may contain up to 5% disseminated and stringer pyrite.

"Delta's expanded land package now covers several fault-bounded sedimentary basins bearing a similar geological setting as the Eureka Gold deposit. The I-Zone sector, covers an area over 4 square kilometres in such a geological setting. The gold mineralization at the I-Zone is somewhat different from that of the Eureka Deposit, but occurs in a similar geological setting, adjacent to the faulted boundary of a sedimentary basin in the southern portion of the expanded property. The Delta team is systematically uncovering new areas with great potential for new mineralization on the newly acquired ground and getting ready to thoroughly test these new targets in 2025," said André Tessier, President and CEO.