Saville Resources Inc. Returns 1.36% Nb2O5 over 4.5 m, Within a Larger Interval of 0.80% Nb2O5 over 31.5 m at the Niobium Claim Group Property, Quebec

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[{"type":"text","content":"Saville Resources Inc. Returns 1.36% Nb2O5 over 4.5 m, Within a Larger Interval of 0.80% Nb2O5 over 31.5 m at the Niobium Claim Group Property, QuebecVANCOUVER, BC / ACCESSWIRE / June 11, 2019 / Saville Resources Inc. (TSXv: SRE, FSE: S0J) (the \"Company\" or \"Saville\") is pleased to announce the most well-mineralized niobium drill hole completed to date to at the Mallard Prospect within its Niobium Claim Group Property (the \"Property\"), Quebec. Sample assays for drill hole EC19-174A have now been received and have returned the strongest and widest mineralized intervals of niobium to date on the Property. Starting from only 17 m depth (core length), results include 0.80% Nb2O5 over 31.5 m, including 0.98% Nb2O5 over 13.5 m or 1.36% Nb2O5 over 4.5 m, as well as a second sub-interval of 1.04% Nb2O5 over 7.7 m. This near-surface mineralization is followed by a second well-mineralized interval, starting from 96.5 m depth (core length), which assays 0.79% Nb2O5 over 37.0 m, including 1.01% Nb2O5 over 7.5 m, as well as a third mineralized horizon assaying 0.67% Nb2O5 over 20.0 m. A total of eleven (11) individual samples from EC19-174A returned >1% Nb2O5 with a peak sample of 1.68% Nb2O5 over 1.5 m.Company President Mike Hodge comments, \"We are absolutely thrilled with the results of our maiden drill program at Mallard. Not only was the first hole of the program better than all the niobium holes completed historically, it was further surpassed by the last hole of the program (EC19-174A), which is the most well-mineralized niobium drill hole to date on the Property. As such, the potential at Mallard has increased considerably as a result of our drilling this past winter, and we are very excited for Phase II as we continue to delineate the mineralized body\".To date, preliminary interpretation of the drill data indicates the Mallard Prospect is characterized by a series of sub-parallel, elongate, moderate-steep dipping, northwest trending mineralized horizons that extend from surface and remain open in all directions. These higher-grade mineralized horizons are separated by comparable horizons of moderate to low grade niobium mineralization. Given the elongate nature of the mineralized horizons, as well as their moderate-steep dip, the mineralized horizons encountered at depth in each hole have a reasonable potential to continue...

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