U3O8 Corp. Reports Uranium-Vanadium Grades from Unconsolidated Gravel and Sand at La Rosada, Laguna Salada District, Argentina

09:00 EST Thursday, January 19, 2017 

TORONTO, Jan. 19, 2017 /CNW/ - U3O8 Corp. (TSX: UWE, OTCQB: UWEFF) ("U3O8 Corp." or the "Company") announces uranium and vanadium assays from exploration trenching of soft gravel and sand in the La Rosada area, which the Company considers to be an extension of the Laguna Salada Deposit.

"Last week we reported that our focus on exploration for higher-grade extensions to the Laguna Salada Deposit had led to the discovery of uranium and vanadium in a layer adjacent to, and beneath, gravel in the La Rosada area," said Dr. Richard Spencer, CEO of U3O8 Corp. "That was an unexpected bonus because our target was uranium and vanadium in the gravel itself, which is an extension of the layer that contains the Laguna Salada Deposit 50 kilometres to the south. Assay results from the gravel at La Rosada, reported in today's release, have grades similar to the very highest-grade material in the Laguna Salada resource.  In addition, the assay results show that uranium in La Rosada gravels can be efficiently concentrated into the fine-grained component of the gravel with the removal of pebbles and coarse sand by screening.  The higher grade, as well as the efficiency of concentration of uranium from La Rosada gravels, has the potential to lower estimated production costs for the Laguna Salada Deposit." 

Assay Results

Table 1.  Summary assay results from composite panel samples from trenches in unconsolidated gravel and sand in the La Rosada area.  

Sample Data

Assay Data

Sample No

Material

From
(metres)

To
(metres)

True
Thickness
(metres)

U 3 O 8 (ppm)

V 2 O 5 (ppm)

Bulk
sample

In Fine
(<0.15mm)
Component
After Screening

Bulk
sample

In Fine
(<0.15mm)
Component
After Screening

16828

Gravel

0.3

0.6

0.3

106

1,304

234

801

16834

0.3

0.7

0.4

5,475

20,764

1,963

7,568

16839

0.4

0.7

0.3

701

1,114

1,326

1,191

16841

0.4

1.2

0.8

154

2,844

322

1,358

16889

0.7

1.7

1.0

133

570

140

623

Average: Mineralized Gravel

0.55

1,314

5,319

797

2,308

16829

Sand

0.6

1.5

0.9

2,800

3,155

1,432

1,573

16831

0.7

1.5

0.8

501

1,113

705

1,380

16832

0.4

1.0

0.6

597

675

669

736

16833

1.0

1.4

0.4

493

1,031

1,054

1,375

16835

0.7

1.3

0.6

388

722

254

396

16836

0.4

1.0

0.6

138

349

263

415

16837

0.8

1.2

0.4

195

533

234

399

16842

1.2

2.2

1.0

699

1,239

841

1,117

Average: Mineralized Area of Sand Layer

0.7

726

1,102

681

924

16830

Sand

0.6

1.6

1.0

76

134

952

970

16874

1.4

2.5

1.1

13

193

103

579

16894

0.4

1.2

0.8

59

114

167

270

Combined Grade & Thickness of Sand and Overlying Gravel in Trenches Where Both Layers are Mineralized:

16828 &16829

Gravel & Sand Layers

0.3

1.5

1.2

2,197

2,692

1,360

1,380

16834 & 16835

0.3

0.7

1.0

2,422

5,732

938

2,194

16841 & 16842

0.4

2.2

1.8

154

1,640

1,326

1,177

Average of Mineralized Gravel and Mineralized Sand Where They Occur in the Same Trench

1.3

1,591

3,355

1,208

1,584

 

Uranium-Vanadium – Bearing Gravel and Sand

Gravel at La Rosada and Laguna Salada have similar general characteristics. At Laguna Salada, however, the gravel forms a tabular sheet deposited in an outwash plain while at La Rosada, gravel occupies northeast- to east-trending channels that are about 150 metres wide, and the one that has been most extensively explored is at least 2 kilometres long (Figure 1).  Similar northeast- to east-orientated trends of radiation measured in radon cups in the area south of La Rosada may be indicative of similar mineralized channels in that area. The channel-constrained distribution of gravel is a feature that La Rosada has in common with the Langer Heinrich Deposit in Namibia.  

A sand layer that lies beneath the gravel at La Rosada may also have been preserved in channel features.  The sand layer is extremely friable, and very significantly, is well mineralized in some areas where it has been exposed in exploration trenches.  The sand layer has characteristics that are similar to the unconsolidated sands that host the Tubas Uranium Deposit in Namibia and represents a target in its own right at La Rosada.  

Uranium-vanadium – bearing rhyolitic volcanic tuff, assay results from which were reported on January 11, 2017, lie adjacent to and beneath the sand layer at La Rosada.   

Beneficiation

The key to the Laguna Salada Deposit is the ease with which the powdery uranium-vanadium mineral, carnotite, can be washed off sand grains and pebbles, concentrating in the fine-grained material.  Gravel at La Rosada shows similar characteristics with carnotite forming a friable coating on pebbles and sand grains – a YouTube video available via this link shows the nature of the gravel and its mineralization at La Rosada.  

The "Bulk Sample" column in Table 1 above provides the overall grade of uranium and vanadium in the gravel and sand samples from La Rosada.  This grade is derived from a large sample in which all the material, including the barren pebbles and sand grains, have been crushed and assayed with the uranium-vanadium – bearing material that coats the grains.  These grades provide the raw data that are necessary for future resource estimation.

The grade of the fine component, composed of grains less than 0.15 millimetres in diameter, that was separated from the pebbles and sand by sieving, has an average grade of 0.5% (5,319ppm)  U3O8, with a sample that spiked to 2% U3O8 (20,764ppm, Table 1).  The average grade of vanadium of the fine material is 0.23% (2,308ppm) V2O5. The average thickness of the gravel is 0.5 metres, with mineralization starting from 0.3 to 0.7 metres below surface.  Only the fine component of the gravel would be processed for uranium and vanadium extraction.  

Results from the unconsolidated sand layer that lies beneath the gravel at La Rosada show that its uranium and vanadium are also concentrated into the fine material by washing and sieving the sand.  The average grade of the sand is 726ppm U3O8 while the fine component has a grade of 1,102ppm (0.1%) U3O8. Vanadium assays average 681ppm in the raw sand and 924ppm V2O5 in the fine component. The average thickness of the sand layer is 0.7 metres.

Where gravel and sand are mineralized in the same trench, the combined average thickness of the uranium-vanadium – bearing layer is 1.3 metres with an average grade, in the fine material, of 0.33% (3,355ppm) U3O8 and 0.16% (1,584ppm) V2O5. 

Estimated Cash Cost of Production at Laguna Salada

The Preliminary Economic Assessment ("PEA")1 modeled mining of the richest areas of the Laguna Salada Deposit followed by successively lower-grade areas so that the capital cost of the Project could be paid off as quickly as possible.  Using the data available at the time of the PEA, this approach resulted in an estimated cash cost of production of US$11.62 per pound of uranium in year one, rising to average US$21.62 per pound over the life of the mine modeled in the PEA (Figure 2).  This graphic shows the relationship between uranium grade and estimated cash cost of production by year established in the PEA on the Laguna Salada Deposit.

Focus of Further Work

The next steps in the drive to lower estimated production costs for the broader Laguna Salada Project are as follows:

• A link between mineralization in the tuff and the overlying gravel observed at La Rosada has led to a better understanding of higher uranium-vanadium grades found at the base of the gravel at Laguna Salada.  With the insight gained from La Rosada, it is considered likely that higher-grade mineralization at the base, where the gravel rests on tuff, represents a second, deeper layer of mineralization that adds further, higher-grade resource potential at Laguna Salada2  that will be explored with trenching and vibrosonic drilling in due course;   


• Continued exploration of higher-grade mineralization in gravel, sand and volcanic tuff in the La Rosada area with the aim of identifying areas that could be cost-effectively included in a future resource estimate; and 


• Metallurgical test work to determine the efficiency of the U-pgrade© processing method to concentrate uranium and vanadium into a smaller mass than is currently being achieved with screening.  With the identification of the uranium-vanadium – bearing sand at La Rosada, the planned test work was delayed in order to incorporate this new style of mineralization. Initial results are now expected in Q2.  

 

Sample Preparation and Assay

Panel samples were taken on the walls of each trench, bagged and delivered to ACME's preparation facility in Mendoza, Argentina.  Each sample was riffle-split.  One sub-sample was crushed, split and pulverized to 75µm and a split of 250 grams sent for assay to provide an assay value for the raw gravel and sand to provide data for resource estimation purposes.  A second set of sub-samples was wet-screened through successively finer mesh starting at 2mm, through 550 micrometres ("µm"), 180µm and finally at 150µm.  Each size fraction was dried in ovens at 60°C and each fraction was sent to ACME's analytical facility in Vancouver, Canada, for analysis by ICP-ES and ICP-MS 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. 

About U3O8 Corp.

U3O8 Corp. is focused on exploration and development of deposits of uranium and associated commodities in South America.  Potential by-products from uranium production include commodities used in the energy storage industry – in the manufacture of batteries - such as nickel, vanadium and phosphate.  The Company's mineral resources estimates were made in accordance with National Instrument 43-101, and are contained in three deposits:  

• 
  Laguna Salada Deposit, Argentina – a PEA shows this near surface, free-digging uranium - vanadium deposit has low production-cost potential; 


• 
  Berlin Deposit, Colombia – a PEA shows that Berlin also has low-cost uranium production potential due to revenue that would be generated from by-products of phosphate, vanadium, nickel, rare earths (yttrium and neodymium) and other metals that occur within the deposit; and 


• 
  Kurupung Deposit, Guyana – a uranium resource has been estimated in four veins within a uranium-zirconium vein system.  Resources have been estimated on four veins, while consistent mineralization of the same type has been intersected in scout drilling of an additional six veins, while yet other veins require first-time exploration drilling.

 

Information on U3O8 Corp., its resources and technical reports are available at www.u3o8corp.com and on SEDAR at www.sedar.com. Follow U3O8 Corp. on Facebook: www.facebook.com/u3o8corp, Twitter: www.twitter.com/u3o8corp and Youtube: www.youtube.com/u3o8corp.

Forward-Looking Statements

This news release includes certain "forward looking statements" related with the development plans, economic potential and growth targets of U3O8 Corp's projects. Forward-looking statements consist of statements that are not purely historical, including statements regarding beliefs, plans, expectations or intensions for the future, and include, but not limited to, statements with respect to: (a) the low-cost and near-term development of Laguna Salada, (b) the Laguna Salada and Berlin PEAs, (c) the potential of the Kurupung district in Guyana, (d) impact of the U- pgradeTMprocess on expected capital and operating expenditures, and (e) the price and market for uranium. These statements are based on assumptions, including that: (i) a ctual results of our exploration, resource goals, metallurgical testing, economic studies and development activities will continue to be positive and proceed as planned, and assumptions in the Laguna Salada and Berlin PEAs prove to be accurate, (ii) a joint venture will be formed with the provincial petroleum and mining company on the Argentina project, (iii) requisite regulatory and governmental approvals will be received on a timely basis on terms acceptable to U3O8 Corp., (iv) economic, political and industry market conditions will be favourable, and (v) financial markets and the market for uranium will improve for junior resource companies in the short-term. Such statements are subject to risks and uncertainties that may cause actual results, performance or developments to differ materially from those contained in such statements, including, but not limited to: (1) changes in general economic and financial market conditions, (2) changes in demand and prices for minerals, (3) the Company's ability to establish appropriate joint venture partnerships, (4) litigation, regulatory, and legislative developments, dependence on regulatory approvals, and changes in environmental compliance requirements, community support and the political and economic climate, (5) the inherent uncertainties and speculative nature associated with exploration results, resource estimates, potential resource growth, future metallurgical test results, changes in project parameters as plans evolve, (6) competitive developments, (7) availability of future financing, (8) exploration risks, and other factors beyond the control of U3O8 Corp. including those factors set out in the "Risk Factors" in our Annual Information Form available on SEDAR at www.sedar.com. Readers are cautioned that the assumptions used in the preparation of such information, although considered reasonable at the time of preparation, may prove to be imprecise and, as such, undue reliance should not be placed on forward-looking statements. U3O8 Corp. assumes no obligation to update such information, except as may be required by law. For more information on the above-noted PEAs, refer to the September 18, 2014 technical report titled "Preliminary Economic Assessment of the Laguna Salada Uranium-Vanadium Deposit, Chubut Province, Argentina" and the January 18, 2013 technical report titled "U3O8 Corp. Preliminary Economic Assessment on the Berlin Deposit, Colombia."

________________________
1 September 18, 2014 technical report:  "Preliminary Economic Assessment of the Laguna Salada Uranium Vanadium Deposit, Chubut Province, Argentina ."   
2 May 20, 2011 technical report:  "Laguna Salada Project, Chubut Province, Argentina, NI 43-101 Technical Report on Laguna Salada:  Initial Resource Estimate".  

 

SOURCE U3O8 Corp.

 

 

U3O8 Corp. Discovers New Style of Uranium-Vanadium at La Rosada, Laguna Salada District, Argentina

09:25 EST Wednesday, January 11, 2017 

TORONTO, Jan. 11, 2017 /CNW/ - U3O8 Corp. (TSX: UWE, OTCQB: UWEFF) ("U3O8 Corp." or the "Company") announces assays from a second type of uranium - vanadium mineralization that occurs in addition to the typical mineralized gravel at La Rosada, an area that lies within the larger Laguna Salada Project in Patagonia, Argentina.

"Our focus is squarely on reducing estimated production costs at the Laguna Salada Deposit," said Dr Richard Spencer, CEO of U3O8 Corp. "One way of achieving that goal is by delineating additional higher grade material - and our exploration team has risen to that challenge by finding high-grade uranium-vanadium in friable volcanic rocks – a type of mineralization that occurs in addition to the gravel-hosted mineralization typical of the Laguna Salada district. Trenching over the last couple of months has shown that uranium-vanadium in the volcanic rock constitutes a target in its own right, adding to the potential of the La Rosada target. Assay results from mineralized gravel at La Rosada will be released in the next few weeks."

Figure 1. Map showing the location of the La Rosada exploration area relative to the footprint of the Laguna Salada resource and the gravel plain in which the mineralization occurs (inset map). The main map shows the location of mineralized tuff (pale blue) and gravel (green).

Assay Results

Table 1. Summary assay results for composite panel samples from the walls of trenches excavated in rhyolitic tuff (volcanic rock) from the La Rosada area. Results from tuff from a prior press release made on November 12, 2013, before the significance of this mineralization was appreciated, are included (shaded grey) for completeness.

Target Area

Sample No

From (m)

To (m)

True
Thickness (m)

Assay Data

U 3 O 8 (ppm)

V 2 O 5 (ppm)

PALA

16876

0.2

1.1

0.9

3,927

1,340

16878

0.5

1.5

1.0

2,331

872

16884

0.3

1.1

0.8

3,125

1,047

Average grade of mineralized zone at La Pala

0.9

3,128

1,086

16881

0.3

1.0

0.7

66

103

16875

0.2

1.0

0.8

106

141

16887

0.7

2.5

1.8

40

84

16936

0.4

1.1

0.7

76

107

16938

0.4

2.1

1.7

76

338

12 ZONE

16854

0.3

1.3

1.0

8,927

3,008

16864

0.7

1.4

0.7

935

571

16867

0.2

1.2

1.0

2,706

1,015

16870

0.9

1.9

1.0

3,051

1,289

16895

0.4

1.4

1.0

405

253

16899

0.4

1.7

1.3

1,172

333

16902

0.4

1.2

0.8

459

265

Average grade of mineralized area at 12 Zone

1.0

2,522

962

16856

1.2

2.2

1.0

243

290

16860

1.5

2.5

1.0

66

201

16862

0.8

1.3

0.5

39

299

16904

0.5

1.2

0.7

209

384

21127

0.4

1.0

0.6

97

289

21139

0.3

0.7

0.4

199

278

23012

0.4

1.0

0.6

200

444

PESCADO
NORTE

21131

0

0.6

0.6

913

377

21134

0

0.9

0.9

861

439

8780

0.5

0.9

0.4

1,730

623

8784

0.1

0.8

0.7

1,956

890

8772

0.2

0.3

0.1

7,933

2,644

Average grade of mineralized zone at Pescado Norte

0.5

2,679

995

16906

0.3

1.1

0.8

109

105

16908

0.3

1.1

0.8

215

246

8778

0.1

0.3

0.2

173

96

8787

0.2

0.5

0.3

157

162

 

Mineralized Zones

Uranium-vanadium is exposed in rhyolitic tuff where the overlying gravel has been eroded at La Rosada. The three zones of mineralization identified to date have a high proportion of carbonate where the tuff has been altered and weathered to form a soft, friable layer that starts anywhere from surface to a depth of 1.5 metres.  

The average thickness of mineralization in the La Pala zone is 0.9 metres with an average grade of 3,128ppm (0.31%) U3O8, with grades ranging between 0.23% and 0.39% U3O8 (Table 1).  Mineralization in the 12 Zone averages one metre thick with an average grade of 2,522ppm (0.25%) with a grade range of 0.04% to 0.9% U3O8. The layer of mineralization at Pescado Norte is thinner, averaging 0.5 metres with an average grade of 2,679ppm (0.27%) and a grade range of 0.09% to 0.79% U3O8.  Vanadium grades are relatively constant at 0.1% V2O5 across the three areas of mineralized tuff.  

The mineralization encountered to date shows lateral continuity over a combined area of approximately 0.4 square kilometres. 

Mineralization in the tuff at Pescado Norte lies in a northeast-trending zone that is aligned with, and may form the extension of, a mineralized channel in the adjacent gravel. The alignment raises the question as to whether there is a link between mineralization in the volcanic rocks and the adjacent gravel.  

There is a possibility that the horizontal mineralized layer in the tuff derives from feeder structures deeper in the tuff – a possibility that will be investigated by drilling as available exploration funding permits.

Beneficiation

Beneficiation characteristics of the gravel at Laguna Salada are good, resulting in concentration of 82% of the gravel's uranium into fine-grained material that constitutes just 9% of the gravel's original weight1, because the barren pebbles and coarse sand can be so easily removed by sieving.  Beneficiation of the tuff, which does not contain pebbles, is likely to be less efficient at concentrating the mineralization; however, this assumption will be confirmed with test work in due course.

Estimated Cash Cost of Production at Laguna Salada (from the PEA)

Since the mineralization at Laguna Salada is contained within a flat sheet lying within three metres of surface, mining could commence at any chosen location. The Preliminary Economic Assessment "PEA") modeled mining of the richest areas of the Laguna Salada Deposit followed by successively lower-grade areas so that the capital cost of the Project could be paid off as quickly as possible.  Using the data available at the time of the PEA, this approach resulted in an estimated cash cost of production of US$11.62 per pound of uranium in year one, rising to average US$21.62 per pound over the life of the mine modeled in the PEA (Figure 2).