International Millennium Mining Corp.: Results from Silver Peak's Winter 2017 Exploration Programs Exceed Expectations

2018-03-05 / @nasdaq

 

VANCOUVER, British Columbia, March 05, 2018 (GLOBE NEWSWIRE) -- International Millennium Mining Corp. (“IMMC” or the “Company”) (TSX-V:IMI) announces that as a result of its recent land acquisitions at Silver Peak, the Company embarked on a winter exploration program, which demonstrated surface gold and silver mineralization was much more extensive than previously anticipated. The Silver Peak property now consists of approximately 4,000 contiguous acres, which hosts fourteen (14) well mineralized fault/vein structures. Two of these structures have so far produced 9.8 million ounces of silver (Ag) and 52.9 thousand ounces of gold (Au).

The winter program focused on sampling ten (10) known fault/vein structures in the 16-to-1 Canyon (see Silver Peak Property Map, on the Company’s website). Table 1 shows the veins that were examined during the work program along with their orientation and known lengths; these lengths represent the exposed occurrence of vein material.

Table 1. Vein Descriptions

Vein Descriptions
 

Zone Name
(Average)Length (m)
Strike (°)Dip (°)VeinHost-Fault
Red Mountain042VerticalMultiple veins2,000
16 to 105575° SE6701,400
Eagle04863° NW9001,200
Chico06575° SE400700
Burney02584° SE400800
Patience05572° SE300700
Kathy038Vertical200?
Elaina19068° SE200?
Merle19250° SE200?
14 to 1UnknownUnknown??

Historical production at the 16-to-1 Mine was from the 16-to-1 Vein and the Colorado Zone, a splay vein. According to historical records, neither of these zones were completely exploited. Seven (7) samples were collected from muck-piles and adits of the 16-to-1 Mine, with sample values ranging from 1.09 to 8.79 g/t Au and 62 to 667 g/t Ag, as shown in Table 2. In this area, at surface, the structures consist of numerous narrow veins that individually are less than 1.5 m wide, but they lie within a wider (10 to 20 m wide) deformed zone containing irregular veining. At a depth of 50 m, it appears from historical work that this veining coalesces into much wider zones of well mineralized material.

Table 2.  16-to-1 Vein Sample Results

16-to-1 Vein Sampling Results
Sample No.VeinDescriptionAu (g/t)Ag (g/t)
M68514516-to-116-to-1 Shaft #1 Muck Pile; grab1.0962
M68514616-to-116-to-1 Muck Pile east of 7200-level Adit; grab2.92505
M68515116-to-116-to-1 Surface NE of Shaft #1; Chip over 1 m1.79195
M68516916-to-1UG in #2 adit 16-to-1; Chip over 1.5 m2.5091
M68517016-to-116-to-1 Surface by #2 Adit; Chip over 1.5 m4.16272
V66150216-to-116-to-1 muck pile grab; dark; 7200-level; grab1.45667
V66150316-to-116-to-1 muck pile grab; light; 7200-level; grab8.79476

The Red Mountain Fault Zone is a major NE-SW trending fault zone, located 100 to 300 m north of the 16-to-1 Vein. With a strike of 042° it is projected to merge with the 16-to-1 Vein west of the 16-to-1 Canyon. Due to the rugged terrain only one sample from a narrow calcite-quartz vein was collected. This sample contained >25% Ca suggesting that it is very high in the epithermal vein system and above the zone where precious metals would be anticipated. Further work is required in this area either with surface drilling or underground development.

In the northwest portion of the property, northeast of the 16-to-1 structure, the 14-to-1 and Eagle Veins were sampled where exposed in old pits, trenches and outcrops. Sample results in these areas did not contain significant mineralization, with sample values ranging from no detectable precious metals to 0.25 g/t Au and 18 g/t Ag, the exception being one significant sample from an outcrop in the eastern projection of the Eagle Vein system on the west side of the 14-1 Canyon. This sample was from a 30 cm wide vein within a veined and deformed structure that was more than 20 m wide and assayed 2.57 g/t Au and 53 g/t Ag despite being dominantly calcite (>25% Ca).

The 2017 Winter program demonstrated that there is significant potential on the west side of the 16-to-1 Canyon, an area that has not been systematically explored to-date, and during the program three strongly mineralized areas were identified in the lower 16-to-1 Canyon, see sample results in Table 3, below. The mineralized zones include the western end of the Chico Vein, which is strongly mineralized at surface where the exposed veining is primarily calcite; the Burney Vein, which is well developed and well mineralized on both sides of the 16-to-1 Canyon, but was never fully explored underground; and the Patience, Kathy, Elaina and Merle Vein Cluster, which are all proximal and oriented in such a way as to suggest that they may merge at a shallow depth, or are related to a common structural feature, such as an intrusive body, at shallow depth. Most of the historical drilling in this region was carried out in the active mining areas in order to locate additional ore reserves. Very little attention was given to other known mineralization in this portion of the Silver Peak Property, partially because of ownership issues during the time when the mine was in operation by Sunshine Mines.

Table 3.  Lower 16-to-1 Canyon Sample Results

Lower 16-to-1 Canyon Sampling Results
Sample No.VeinDescriptionAu (g/t)Ag (g/t)
M685178ChicoChico Vein; upper0.6437
M685179ChicoChico Vein B1.23148
M685180ChicoChico Vein A1.5056
M685181ChicoChico Vein C0.7446
M685182ChicoChico 1 wide1.19129
M685183ChicoChico Vein above Polvorin1.1257
M685150BurneyBurney Vein; old, open cut, Chip over 3 m0.2133
M685184BurneyBurney Vein NE; 50 cm of 3m vein0.1213
M685185BurneyBurney Vein system, 20 cm vein0.9686
M685186BurneyBurney SE; 30 cm of a 2 m wide zone0.3127
M685187BurneyGrab of Burney Vein in 3m open cut0.1015
M685188BurneyBurney 40cm 060 Vein1.0570
M685190BurneyBurney South Adit; Middle, chip over 1m1.3849
M685191BurneyBurney South Adit; Left, chip over 1m3.7975
M685192BurneyBurney South Adit; Right, chip over 1m0.1716
M685189MerleMerle North; 20+5 cm2.2918
M685193PatiencePatience 30 cm0.3349
M685194KathyKathy Vein; 3m wide -65° at 030°0.2521
M685195PatiencePatience0.5164
M685198MerleMerle Vein; 40 cm0.3125
M685199MerleMerle Vein; 50 cm0.4125
M685200ElaineElaina Vein0.30<5
V661501ElainaElaina Vein; 20 cm0.7013

The host vein material located within the Silver Peak Project area are classic epithermal veins. The veins display distinct vertical zoning, consisting principally of quartz and adularia at the bottom, and calcite and gypsum nearer the surface. In addition, the upper parts of the vein systems in this area have been weathered and leached near surface and oxidized to depths of 200 to 300 meters. The higher grades of known Ag and Au mineralization appear to occur within the interval from 50 meters below surface to the base of the oxidized zone, a distance of 150 to 250 metres. Below that point, grades of Cu, Pb and Zn appear to increase and precious metals decrease, although there is very little drill data from below the oxidized zone to assess the economic viability of these zones. As a general rule, the mineralized veins in the Silver Peak Project area are narrow in surface exposures, but increase dramatically in width a short distance down dip. Drilling is required to further delineate the potential of this area.

Seymour Sears, P. Geo, the Company’s consulting geologist since 2004, completed the Silver Peak Winter geology field work program in late December 2017. The Company is currently planning its 2018 drilling program, which is anticipated to begin following receipt of a temporary water use permit from the Nevada Division of Water Resources.

International Millennium Mining Corp. (TSX-V:IMI) is focused on the acquisition, exploration and development of precious metal deposits in the Americas, such as its Silver Peak silver-gold project in southwest Nevada. The Company’s common shares trade on the TSX Venture Exchange under the symbol: IMI and on the Frankfurt Exchange under the symbol: L9J.

Seymour Sears, P.Geo, a qualified person as defined by Nation Instrument (“NI”) 43-101, reviewed and approved the technical information contained in this news release.

ON BEHALF OF THE BOARD

”John A. Versfelt”

John A. Versfelt
President and CEO

Further information about the Company can be found on the Company’s website (www.immc.ca) and SEDAR (www.sedar.com) or by contacting Mr. John Versfelt, President & CEO of the Company at 604-527‑8135.

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. This news release may contain forward-looking statements including but not limited to comments regarding the timing and content of upcoming work programs, geological interpretations, potential mineral recovery processes and other business transactions timing. Forward-looking statements address future events and conditions and therefore, involve inherent risks and uncertainties. Actual results may differ materially from those currently anticipated in such statements.                                 

CONTACT: John A. Versfelt, President & CEO
Telephone: (604) 527-8135
E-mail: info@immc.ca

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