30.10.2018

Tudor Gold Continues To Grow Copper Belle; Hole 37b Returns 482 m of 0.486 g/t gold, including 175.5 m of 0.790 g/t gold

Vancouver, British Columbia--(Newsfile Corp. - October 30, 2018) - Tudor Gold Corp. (TSXV: TUD) (FSE: TUC) (the "Company" or "Tudor Gold") is pleased to
report results from four holes of the nine-hole 2018 drill program on the Copper Belle zone of the Company's Treaty Creek property, in the "Golden
Triangle" area of north-western BC.

The deep drilling program is now finished for the season and results of core sampling have been received for six of the nine holes completed. The first two
holes were reported in the August 23 news release. 
Walter Storm, President and CEO, stated: "As the assay results come in from our deep drilling program at Copper Belle, the gold mineralized zone is really
taking shape. We are seeing thick intervals of good gold grades in our northernmost hole reported to date. This indicates to us that the strong
Copper Belle mineralization may continue to the north-northeast of our current drilling.

Holes CB-18-34 and 37B were drilled to the northwest at angles of approximately 75 degrees into the central part of a strong magnetic high (see
map below) and returned broad intervals of gold mineralization. Holes CB-18-33B and 35B, located approximately 150 m farther to the west, were also
drilled northwesterly; however, the gold values were lower in these two holes. The objective of the 2018 drill program was to better define the extent of the
Copper Belle zone and the results from these holes have accomplished that. Excellent gold intercepts from our northernmost hole reported to date and
moderately strong magnetic intensity extending north-northeasterly from the north end of the drill grid, indicate that the zone has good potential to
continue in that direction.

Gold, silver and copper results for holes CB-18-33B, CB-18-34, CB-18-35B and CB-18-37B , as well as hole 37, which was lost at 131.2 m, but re-drilled as
37B, are summarized in the table below. CB-18-34 had two wide intervals of gold mineralization; 0.554 g/t Au over 178.5 m, which included 0.830 g/t Au over 75.0 m and a lower zone of 0.344 g/t
Au over 94.5 m. The gold  mineralized intervals are primarily hosted by andesitic tuff and fragmental rocks that are moderately silicified, chlorite
and sericite altered, and cut by abundant fine quartz-carbonate veins. Pyrite content averages about 10%, occurring as disseminations and local coarse
masses in the host rocks, as well as within some of the quartz-carbonate veins, with rare chalcopyrite and arsenopyrite.

CB-18-37B also intersected two zones of mineralization over impressive widths; the upper zone averaged 0.772 g/t gold over 43.5 meters and the lower zone
returned 0.486 g/t Au over 482.0 m, which included intervals of stronger alteration and mineralization, such as 0.790 g/t gold over 175.5 meters.  The
host rocks are similar to those in hole CB-18-34 and higher gold grades are associated with increased silicification, potassic alteration and pyrite
content.

The nine holes drilled in 2018 covered an area measuring approximately 370 meters by 250 meters, to depths of 600 to 900 meters. Based on the wide gold
intervals received to date, the results are expected to considerably increase the range of potential ounces of gold from the 1.8 to 1.9 million ounces
contained within 50 to 45 million tonnes grading 1.12 to 1.35 g/t Au determined from the drill results prior to 2018. A new range of gold ounces
and grades will be determined, incorporating all drill results to the end of 2018 drilling, once the final assays are received and compiled.

The 2018 drilling has now extended the known length of the porphyry-style mineralized system for over 1100 meters. For locations of the 2018 and other
holes in the Copper Belle area that are overlain on Total Magnetics contours, please view the map below. The Copper Belle zone has an elongate
north-northeast trend, dipping at a relatively flat angle to the northwest. Mineralization may be related to an extensive north-northeast trending
tectonic zone, similar to the distribution of the four KSM deposits on Seabridge's property that are located along a ten kilometer length of the
Sulphurets Thrust Fault zone.

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