U308 Corp. Announces Definition of Additional, Higher-Grade Uranium-Vanadium Layers atLaguna Salada Argentina.
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Feb 07, 2017 09:15PM
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U3O8 Corp. Announces Definition of Additional, Higher-Grade Uranium-Vanadium Layers at Laguna Salada, Argentina
Toronto, Ontario - February 7, 2017 - U3O8 Corp. (TSX: UWE), (OTCQB: UWEFF)("U3O8 Corp." or the "Company") announces that, building on the recent discovery of higher-grade uranium-vanadium mineralization at La Rosada, similar channels have been delineated in, and beneath, the lowermost gravel layer at Laguna Salada. These levels are in addition to the layer of mineralization on which the resource estimate[1] was based and may represent significant resource growth potential at Laguna Salada.
"By applying what we have learned from the discovery of higher-grade uranium-vanadium in the La Rosada area, announced in the last few weeks, our exploration team has identified similar higher-grade layers at the base of the gravel, and beneath the gravel, at Laguna Salada," said Dr. Richard Spencer, CEO of U3O8 Corp. "The identification of higher-grade potential provides an opportunity to further reduce estimated production costs for the Laguna Salada Deposit. In addition, it opens up new targets for shallow uranium-vanadium mineralization in soft gravel, sand and silt that can be inexpensively explored through trenching.
Assay Results
Table 1. Summary assay results from composite panel samples from trenches at the base of the unconsolidated gravel, sand and silt layers at Laguna Salada. The extent to which Laguna Salada gravel can be beneficiated, as per Preliminary Economic Assessment (PEA)[2] is also shown for reference.
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Uranium-Vanadium - Bearing Layers at the Base of the Gravel at Laguna Salada
Uranium-Vanadium at Laguna Salada constitutes a "caliche" deposit - where uranium and vanadium precipitated as a result of intense evaporation in a semi-desert environment. Mineralization is concentrated in a layer that is parallel to the surface from which evaporation occurred. Over 90% of the trenches that were used to estimate the resource at Laguna Salada are from a layer of mineralization that is parallel to the surface at shallow depth - constituting typical caliche-style mineralization in the gravel plain.
Trenches excavated at the edge of the plain, where the upper part of the gravel has been removed by erosion, exposed higher-grade mineralization at the base of the gravel. This was considered to be part of the layer of caliche mineralization that simply draped the topography from which evaporation occurred - and was modelled as a single layer in the initial resource estimate at Laguna Salada.
Exploration of the La Rosada area (press releases made on Jan 11th and 19th, 2017 - the latter with video footage of the mineralization in the trenches) revealed, not only well mineralized gravel, but also an underlying, mineralized sand layer and mineralized volcanic material. With the La Rosada discoveries as a model, the exploration team revisited the lower part of the gravel at Laguna Salada and recognized a very similar situation that can be summarized as follows (Figure 1):
There is a possibility that each of these three layers represents a zone of mineralization in its own right that is separate and distinct from the true "caliche" mineralization located in the upper part of the gravel on which the resource estimate is based.
Exploration Targets
Several target areas have been identified for exploration for additional higher-grade resource potential:
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Figure 1. Map showing the location of the gravel plain that contains the Laguna Salada resource (footprint shown in blue), the La Rosada exploration area, and the area that has been covered with a radon cup survey. The target areas for additional higher-grade channels in the lower part of the gravel are shown in red.
Sample Preparation and Assay
Channel samples were taken on the walls of each trench, bagged and delivered to the ALS Chemex' preparation facility in Mendoza, Argentina. Each sample was riffle-split. One sub-sample was jaw-crushed to <2mm and then riffle-split again and a 250 gram sub-sample pulverized to 75µm for shipment to ALS Peru for assay by ICP (method ICP-MEMS61) after four-acid digestion.
Technical Information
Dr. Richard Spencer, P.Geo., CGeol., President and CEO of U3O8 Corp. and a Qualified Person as defined by National Instrument 43-101, has approved the technical information in this news release relating to the Laguna Salada Deposit and the related PEA.
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