Aurania Provides Update on Drilling & Conference Call Details

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Toronto, Ontario--(Newsfile Corp. - November 24, 2021) - Aurania Resources Ltd. (TSXV: ARU) (OTCQB: AUIAF) (FSE: 20Q) ("Aurania" or the "Company") reports that drilling successfully intersected the targeted silver-zinc mineralized layer at Tiria-Shimpia in drill hole SH-004 and assays are awaited. Progress is also being made with exploration for sediment-hosted copper at the Tsenken target in the Company's Lost Cities - Cutucu Project area ("Project") in southeastern Ecuador. Copper has been intersected in several sedimentary layers and targets were refined during a week-long site visit by a specialist in sediment-hosted copper, zinc and lead, Professor Gregor Borg, his third visit to the Project.

Aurania's Chairman and CEO, Dr. Keith Barron and President, Dr. Richard Spencer will be hosting a webcasted exploration update conference call on Friday, November 26, 2021, to discuss recent developments. The webcast link and dial-in details for the conference call are listed below.

Conference Call & Webcast Details

Date and time: November 26th at 11:00am ET.
Webcast URL: Click here to join the webcast.

When prompted, webcast participants enter: First Name, Last Name, Company, Email Address.

Participant Telephone Numbers*

Canada/USA Toll Free: 1-800-319-4610
Toronto Toll: +1-416-915-3239
UK & Europe Toll Free: 0808-101-2791

*Callers should dial in 5 - 10 min prior to the scheduled start time and simply ask to join Aurania's call.

Drilling at Tiria-Shimpia

Drill hole SH-004 at Tiria-Shimpia intersected the zinc-bearing mineralized layer as planned at the location indicated in the press release dated October 28, 2021. Assay results are expected in December and will be press released at that time.

Drilling at Tsenken

A breakthrough has been made in the exploration for sediment-hosted copper with the recognition, confirmed and elaborated on by Prof. Borg, of evidence for evaporite layers, which contain salt and sulphates, within the red-beds at Tsenken and in the limestones at Tiria-Shimpia. Evaporites are the end products of evaporation of saline lakes in desert conditions. A modern analogue would be Israel's Dead Sea. Evaporites are critical in our model to the formation of copper, silver and zinc deposits, as described below.

TSN1-008 has been completed and drill hole TSN1-009 is scheduled to start within days. Final results have been received for TSN1-007.

Results and their context are as follows:

Hole TSN1-007:

  • Hole TSN1-007 confirms continuity of mineralization from surface to depth.

  • The grade of a mineralized sedimentary layer that lies adjacent to an evaporite-related unit at surface, was 1.9% copper and 3 grams per tonne ("g/t") silver and the same layer, intersected at 157m down-hole, contains 0.5% copper over an interval of 1.7 metres ("m"). Both are partial results because the mineralization has been weathered (Figure 1). Weathering results in the formation of acid that would have dissolved and removed copper from the sedimentary layer. To establish the true grade of this sedimentary layer, it would have to be intersected below the weathered layer that reaches a depth of at least 120m below surface, illustrated in Figure 2, in the tropical, high rainfall environment of the Project.

  • The lower part of the drill hole cut a 26m thick evaporite layer. Evaporite is an important component to sediment-hosted mineralization because it forms a seal against which metal-bearing fluids dam, and many deposits are located against such barriers. Evaporite also provides a source of sulphate that would cause the metals to be deposited as sulphides, the form in which metals are found in most sediment-hosted deposits.

  • True to this exploration model, pyrite was intersected immediately beneath the evaporite layer in hole TSN1-007, confirming that the process of fluids carrying metal, in this case, iron, reacted with the sulphate in the evaporite to form iron sulphide (pyrite). This validates the exploration model, confirming the central role that evaporites play in causing metals to precipitate. Copper mineralization beneath this specific evaporite layer is likely to be located closer to the fault that fed metal-bearing fluids into the sedimentary layering. Drill hole TSN1-009 has been sited adjacent to the feeder fault system.

  • This is the second time that continuity of mineralization has been confirmed; the first was in hole TSN1-003 where an intercept of 1m at 0.5% copper and 4g/t silver represents the extension of a mineralized layer sampled at surface. Although not economic, this result provides support for the exploration model and is a vector that helps refine the target area in which higher copper grades should lie.