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The Naarst uranium deposit lies within an extensive zone of uranium anomalies extending for many kilometres within the Sainshand Basin graben in the southeastern Gobi region in Mongolia. The sedimentary units of the graben filling, Late Cretaceous age, Sainshand-Binshiren (Cenomanian to Santonian) packages seem to be the predominant host for the uranium. Locally, roll front enrichment has occurred,...
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