September 15, 2017
Vancouver, B.C.

TUDOR GOLD Reports Preliminary Assay Results in Golden Triangle, BC

TUDOR GOLD Corp. (TSXV: TUD) (FSE: TUC) (the “Company” or “TUDOR GOLD”) today announced that the HC mineralized zone of the HC deposit (the “HC Zone”) within the GR2 claim block on the 60%-owned Treaty Creek project located in the “Golden Triangle, BC” (the “Treaty Creek Project”) hosts a precious metal-rich, polymetallic, volcanogenic massive sulphide and sulfosalt (“VHMS”) mineralized system.
Walter Storm, President and CEO, stated: “We are very pleased with the results so far. We were attracted to the Treaty Creek Project by the clear potential for extensive mineralized zones on our claims and the results from the HC Zone within the GR2 claim block have exceeded our expectations. We look forward to the completion of a resource estimate on the HC Zone, and a resource estimate on the Copper Belle project which is also well underway.” The HC Zone appears to be a complete precious metal-rich VHMS deposit in which the feeder vein system, the vent structures, and the sulphides in a restricted sedimentary basin had been intersected. All three zones of the HC deposit carry elevated values of gold. The feeder vein system also carries elevated silver and base metal (Pb, Zn, Cu) content.
We are very pleased with the results so far. We were attracted to the Treaty Creek Project by the clear potential for extensive mineralized zones on our claims and the results from the HC Zone within the GR2 claim block have exceeded our expectations.

Walter Storm, President and CEO

The HC Zone shows elevated concentrations of gold, silver, Sb-sulfosalts hosted between a pervasively sericite-pyrite-chlorite altered volcaniclastic sequence (bimodal mafic-felsic affinity), and restricted sedimentary basins where mudstones host sulfide mineralization underlying stockwork base metal and precious metal veins. These characteristics are similar and unique to the nearby Eskay Creek deposit. The highest grade, and most continuous precious-metal mineralization within the HC Zone, occurs as an apparent stratabound zone at the contact of the footwall mudstone and the hydrothermally altered volcaniclastic sequence. This is interpreted as being the product of a mineralizing growth-graben fault, proximal to felsic flows, ash tuffs, and felsic conglomerates.

During the ongoing 2017 season, TUDOR GOLD has drilled 13 holes in the vicinity of, and to the north of the 9 holes drilled in 2007 and 11 holes in 2009 by American Creek Resources. Together, these 33 holes have produced consistent geology demonstrating the continuity of the feeder vein system, the vent structure, and the sedimentary basin within the area bounded by these holes (assays received up to HC-17-07, awaiting assays on all remaining 2017 holes).

The holes drilled by TUDOR GOLD and American Creek Resources cover approximately 400m along strike and 450m down dip at 50m space increments in the direction of the main mineralized structure. Historical surface sampling carried out by previous operators to both the north and south of the HC Zone indicates that the main mineralized structure extends at least for 3,000m along strike. The entire 3,000m mineralized structure which hosts HC remains open to the north, south beyond the existing drill holes, and down dip.

Assay results

The Feeder Vein System

It is comprised of discordant veins hosted mainly in pervasively sericite-pyrite-chlorite altered volcaniclastic sequence. Two types of veins are recognized: silver dominant Mn-rich carbonates and sulphides (semi-massive yellow to light brown zoned sphalerite, galena, pyrite and minor chalcopyrite can add to >50% of the veins) and gold dominant chalcedonic quartz veins. Textures include those more typical of the epithermal suite (banded, crustiform, breccia/vein).

The Feeder Vein System

Hole IDFrom (m)To (m)Interval (m)Au (ppm)Ag (ppm)
HC-17-02256.65257.45 0.84.5355.1-
and435.3435.80.533.80 -

* True thickness of the different mineralized intervals still to be determined.

The Vent Structure

It is comprised of silica flooded and altered mudstone and volcanic conglomerates along with breccias and semi-massive sulphide replacements. Several stages of silica can be recognized cementing and replacing successive events of brecciation. Silica alteration occurs as silicification and chalcedonic silica, usually gray to bluish in color, obliterating previous textures. Pyrite and Sb-sulphosalts are the dominant sulphides as veinlets, stringers and semi-massive replacements. Stibnite, galena, sphalerite and arsenopyrite are also common in veinlets and disseminations

Assay results vent system

Hole IDFrom (m)To (m)Interval (m)Au (ppm)

* True thickness of the different mineralized intervals still to be determined.

The Sulphides in Sedimentary Basins

Fine grained pyrite and Sb-sulphosalts have been identified as finely laminated sedimentary beds and patchy pyrite/quartz replacements within mudstones/siltstones in the proximity of the venting structures intersected in core, particularly around holes HC-17-01, 04, 05, 08, 10, 11 and 12 (as per visual inspection of the drill core). The mineralization appears to be hosted in the immediate contact of the underlying footwall mudstone unit and the upper altered volcaniclastic sequence.

Assay results sulphides in mudstone host

Hole IDFrom (m)To (m)Interval (m)Au (ppm)

* True thickness of the different mineralized intervals still to be determined.

Quality Control and Data Verification

Samples were assayed by Activation Labs in Kamloops, BC. Analytical accuracy and precision are monitored by the submission of blanks, certified standard samples and duplicate samples inserted at regular intervals into the sample train by TUDOR GOLD personnel. Activation Lab’s quality system complies with the requirements for the International Standards ISO 9001: 2000 and ISO 17025: 1999.

Qualified Person

This press release has been prepared and verified by Raul Sanabria, M.Sc., P.Geo, EurGeol, Exploration Manager and Qualified Person for the 2017 Treaty Creek Project field season and a Qualified Person for the purposes of National Instrument 43-101.


TUDOR GOLD is a precious and base metals explorer with properties in British Columbia’s Golden Triangle, an area that hosts producing and past-producing mines and several large deposits that are approaching potential development. The 17,913 hectare Treaty Creek project (in which TUDOR GOLD has a 60% interest) borders Seabridge Gold Inc.’s KSM property to the southwest and borders Pretium Resources Inc.’s Brucejack property to the southeast. The Company also has a 100% interest in the Electrum Project, earn in options and 100% interests in other prospective projects located in the Golden Triangle area.

Contact Information

Cathy Hume

CHF Capital Markets

Phone:416-868-1079 Ex 231

Aris Morfopoulos

Financial Relations


Cautionary Statements regarding Forward-Looking Information

Certain statements contained in this press release constitute forward-looking information. These statements relate to future events or future performance. The use of any of the words “could”, “intend”, “expect”, “believe”, “will”, “projected”, “estimated” and similar expressions and statements relating to matters that are not historical facts are intended to identify forward-looking information and are based on the Company’s current belief or assumptions as to the outcome and timing of such future events. Actual future results may differ materially. 

All statements other than statements of historical fact included in this release, including, without limitation, statements regarding analysis and re-interpretation of data, and potential mineralization and geological merits of the Treaty Creek Project and other future plans, objectives or expectations of the Company are forward-looking statements that involve various risks and uncertainties. There can be no assurance that such statements will prove to be accurate and actual results and future events could differ materially from those anticipated in such statements. Forward-looking statements are based on a number of material factors and assumptions. Important factors that could cause actual results to differ materially from Company’s expectations include actual exploration results, changes in project parameters as plans continue to be refined, results of future resource estimates, future metal prices, availability of capital and financing on acceptable terms, general economic, market or business conditions, uninsured risks, regulatory changes, defects in title, availability of personnel, materials and equipment on a timely basis, accidents or equipment breakdowns, delays in receiving government approvals, unanticipated environmental impacts on operations and costs to remedy same, and other exploration or other risks detailed herein and from time to time in the filings made by the Company with securities regulators. Although the Company has attempted to identify important factors that could cause actual actions, events or results to differ from those described in forward-looking statements, there may be other factors that cause such actions, events or results to differ materially from those anticipated. There can be no assurance that forward-looking statements will prove to be accurate and accordingly readers are cautioned not to place undue reliance on forward-looking statements. Neither TSX Venture Exchange nor its Regulation Services Provider (as that term is defined in the policies of the TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of this release.