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Ximen Mining Updates Exploration Results Gold Drop Project Historic Greenwood Mining Camp

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Ximen Mining Updates Exploration Results Gold Drop Project Historic Greenwood Mining Camp

 

 

 

 

 

Ximen Mining Corp. (TSX-V:XIM) (FRA:1XMA) (OTCQB:XXMMF) is pleased to announce the last assay results from 2019 obtained by its option partner GGX Gold Corp. at the Gold Drop property in the Greenwood Mining Camp. Results are provided for the last hole drilled on the COD vein, surface prospecting samples, and the deep drill hole that tested a large geophysical anomaly.

 

The last hole drilled on the COD vein, Hole COD19-49 was drilled to test the COD vein at depth below other holes drilled in 2019. This hole intersected two quartz veined zones containing pyrite that have elevated gold contents. The results are provided in the table below.

 

 

Hole   From     To     Length (m)     Gold (g/t)     Silver (g/t)     Tellurium (ppm)   Description
COD19-49     119.27       119.84       0.57       2.48       24.2       9.7   Quartz veinlets, pyrite
COD19-49     128.62       129.06       0.44       3.33       4.7       13.7   Quartz veinlets, pyrite
                                                   

 

Prospecting was done to evaluate targets for trenching and drilling in 2020. One sample assayed 55.8 grams per tonne gold, 379 grams per tonne silver and 270 ppm tellurium. This grab sample was from a previously unknown occurrence of frost-heaved blocks of vein quartz containing pyrite. This site is a priority for follow-up trenching.

 

Hole AMT19-01 was a designed to test a large geophysical anomaly and was drilled to a depth of 718.8 meters (2,358 feet). The core was logged for geological features and sampled at intervals ranging up to 3.05 meters in length. Geochemical results indicate elevated copper, zinc and iron between 90.31 and 718.7 meters (628 meters). Copper values averaged 249 ppm Cu in 38 of 62 samples that contained 100 ppm or greater copper, with values ranging from 102 to 837 ppm Cu. The highest copper value was for a 0.32 meter sample at 714.06 meters depth, where sulphide mineralization (pyrrhotite and pyrite) was observed. Zinc averaged 175 ppm Zn in 48 of 62 samples containing ppm 100 or greater zinc, with values ranging from 102 to 572 ppm Zn. Iron averaged 10.0% Fe in 48 of 62 samples containing 5% or greater iron, with values ranging from 5.27 to 12% Fe.

 

The elevated values for copper, zinc and iron are associated with calc-silicate altered rocks and magnetite mineralization in the drill core. These features are interpreted as weak, skarn-type mineralization formed by iron-rich fluids that also carried copper and zinc. Historically, skarn-type copper-gold deposits were the main source of metals produced in the Greenwood camp. The Phoenix deposit produced 28,341 kg of gold, 183,036 kg of silver and 235,693 tonnes of copper and the Motherlode produced 6,648 kg gold, 22,083 kg silver, and 34,918 tonnes copper.

 

Skarn mineralization typically occurs at or near the margins of porphyry-type intrusions, which likely generated metal-rich hydrothermal fluids that replaced and reacted with calcareous rocks (limestone or dolomite). Porphyry dikes were intersected in hole AMT19-01, and although calcareous units were not seen in the core, limestone is known to be a minor component of the Knob Hill Group, through which this drill hole passed. Hence the geological environment is favourable for skarn deposits. The alteration and mineralization are interpreted as distal since they are weakly developed. The conclusion is that the hole passed through a skarn-type magnetite calc-silicate replacement zone, possibly on the periphery of a larger skarn deposit. Hole AMT19-01 may have intersected the edge of a major skarn deposit that is yet to be identified.

 

Further investigations will be done, including petrographic studies of the alteration minerals. A review of the geophysical results is also planned. Additional geophysical surveying may be done prior to drilling additional holes. Note that hole AMT19-01 was the first of three holes originally planned to target the geophysical anomaly (see image below).

 

Location of hole AMT19-01, geophysical anomaly boundary (red) and location of C.O.D. veins (green).

 

Analytical results reported above were provided by ALS Laboratories in North Vancouver, BC., which is an independent and accredited commercial laboratory. Analyses for gold were done by fire assay with AA finish on 50 gram sub-samples, or by metallics sieve analyses. Analyses for silver and tellurium were by four acid digestion with ICP-MS finish. Silver results greater than 100 ppm, and Tellurium results greater than 500 ppm, were reanalyzed using a four-acid digestion and ICP-AES or AAS finish on a 0.4g sub-sample. Quality control was monitored using analytical results for reference standards and blank samples inserted into the sample stream at a frequency of 5% each.

 

Dr. Mathew Ball, P.Geo., VP Exploration for Ximen Mining Corp. and a Qualified Person as defined by NI 43-101, approved the technical information contained in this News Release.

 

About Ximen Mining Corp.

 

Ximen Mining Corp. owns 100% interest in three of its precious metal projects located in southern BC. Ximen`s two Gold projects The Amelia Gold Mine and The Brett Epithermal Gold Project. Ximen also owns the Treasure Mountain Silver Project adjacent to the past producing Huldra Silver Mine. Currently, the Treasure Mountain Silver Project is under a option agreement. The option partner is making annual staged cash and stocks payments as well as funding the development of the project. The company has recently acquired control of the Kenville Gold mine near Nelson British Columbia which comes with surface and underground rights, buildings and equipment.

 

Posted January 7, 2020

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