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The Sagvoll project is located northeast of the Norwegian city of Trondheim. The Sagvoll licenses contain 9 separate historic mining areas within license, where copper and other metals were mined in the 19th and early 20th centuries. Historic production focused on copper, with limited attention paid to zinc and gold. Zinc and gold were not assayed by historic operations. Several mines show zinc-rich styles of mineralization, and many of the mine dumps are rich in discarded zinc mineralization.

The geology consists of Cambrian to Ordovician age marine metasediments and metavolcanic sequences of the Trondheim Nappe Complex. there are two types of mineralization at Sagvoll:
•Stacked VMS-style lenses within the Fondsjo Group.
•Gabbroic intrusion-hosted magmatic nickel-copper sulfide within the Gula Group.

VMS style mineralization is developed throughout the areas of historic mine workings, and along extensive geophysical anomalies that extend for over 25 kilometers along strike of the mine workings. Also present in the southeastern portion of the license area are historic nickel-copper sulfide mines and prospects. The Sagvoll project is available for partnership.

Note: The nearby mines and deposits in the region provide context for EMX’s Project, but this is not necessarily indicative that the Project hosts similar mineralization.


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1NGU Deposit Factsheet 1721-018. 2NGU Deposit Factsheet 1721-016. Updated March 2006. 3Falconbridge Geochemical Data. Collected in 2005. 4NGU Deposit Factsheet 1721-010. Updated March 2013.  Updated March 2006. EMX has not performed sufficient work to verify the published historical assay and sampling data, and these data cannot be verified as being compliant with NI43-101 standards. These data should not be relied upon until they can be verified. However, EMX considers these data as reliable and relevant.