Aurania Develops New Copper-Silver Exploration Concept

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Toronto, Ontario--(Newsfile Corp. - May 17, 2019) - Aurania Resources Ltd. (TSXV: ARU) (OTCQB: AUIAF) (FSE: 20Q) ("Aurania" or the "Company") announces that the Company has reassessed the exploration model for the discovered copper-silver mineralization on the Lost Cities-Cutucu Project ("Project") in Ecuador in light of new observations from the field.

The sedimentary-hosted copper-silver mineralization found to date by Aurania is regional in nature and stratigraphically confined to key horizons of carbon-bearing sediments that have been verified in outcrop to extend for a minimum of 22 km (open along strike) across the Project area. There are few geological models that could account for this already very significant lateral extent.

Aurania's Chairman and CEO, Dr. Keith Barron commented, "In October of last year our geologists, tasked to carrying out rather routine stream sediment collection, started to bring an extraordinary array of copper-mineralized large boulders and slabs in from the jungle. Some of these samples were covered in vivid green chrysocolla and malachite, with azurite, cuprite and even native copper as well as more drab chalcocite and tenorite. At first, we treated these as a curiosity, and believed they were related to the supergene weathering of nearby porphyries. However, the copper minerals were hosted exclusively in well-bedded siltstone, mudstone, sandstone and shale, particularly in pieces showing abundant carbonaceous plant fragments, and not in porphyry."

"Our geologists, together with our President, Dr. Richard Spencer, traced these boulders back to outcrops, over what is now a strike length of 22 km. The copper mineralization appears to lie above a red-bed sequence of quartzose sediments in an overlying sequence of black shale with abundant carbonaceous plant trash (Figure 1). The setting is strongly reminiscent of the mineralized zones in the Kupferschiefer ("copper shale"), currently mined by KGHM in Poland."

Exploration Concept

The general model for mineralization in the Kupferschiefer and the Central African Copperbelt of Zambia and the Democratic Republic of the Congo is that copper leached from the sedimentary basin remains in solution because of the oxidised state of the red sandstones ("red-beds"). Saline fluids from salt layers or domes within these sedimentary basins increase the solubility of copper, which forms stable, soluble copper-chloride complexes. Numerous salt domes are associated with the Jurassic red-beds in southeastern Ecuador. Salt is currently produced from two small artisanal operations on the Project. When these basins are reactivated, the saline, copper-bearing fluids flow along the layering of the rock sequence to the faults, which constitute barriers to the fluids, and the fluids tend to rise along these permeability barriers. Where the fluids come into contact with reduced sedimentary layers, such as carbon-bearing black shale or limestone, the copper precipitates.