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Nine Mile Metals Ltd C.NINE

Alternate Symbol(s):  VMSXF

Nine Mile Metals Ltd. is a Canada-based mineral exploration company. It is focused on critical mineral exploration (CME) of volcanic massive sulfide (VMS) (Cu, Pb, Zn, Ag and Au) exploration in the Bathurst Mining Camp, New Brunswick, Canada. It is engaged in exploration of its four VMS projects: Nine Mile Brook VMS; California Lake VMS; Canoe Landing Lake (East-West) VMS and the Wedge VMS Projects. The Nine Mile Brook property covers over 43.98 square kilometers (km2) and is located 10 kilometers southwest of the Brunswick 12 mine. The California Lake VMS Project covers 31.16 km2 and is located north of the Canoe Landing Lake Project and includes a section of the highly prospective Spruce Lake Formation. Its Canoe Landing Lake (East-West) VMS Project covers 10.82 km2 and has nine occurrences/deposits, which is located three km northwest of Canoe Landing Lake. It owns additional 5.06 square kms and 23 claim units adjacent to its California Lake VMS Project.


CSE:NINE - Post by User

Post by Betteryear2on Dec 08, 2023 11:16am
55 Views
Post# 35774912

Nine Mile Metals Provides Drilling Update

Nine Mile Metals Provides Drilling Update

VANCOUVER, British Columbia, Dec. 08, 2023 (GLOBE NEWSWIRE) -- NINE MILE METALS LTD. (CSE: NINE, OTCQB: VMSXF, FSE: KQ9) (the “Company” or “Nine Mile”), is pleased to provide an update on its current drill hole (CL23-10-01) at its California Lake VMS Project.

  • Drill hole is currently at a depth of 433.3 meters, now targeting Lens A at a measured depth of 720m.
  • The Azimuth and Dip are monitored daily, the Azimuth presently at 207 degrees and the Dip flattened to 67 degrees. Our calculations show we are still on target. (Figure 2)
  • Rocks intersected to date include felsic volcanics of the Flat Landing Brook Formation which hosts numerous VMS mines and occurrences in the southern portion of the Bathurst Ming Camp (“BMC”) including the Stratmat and Headway VMS Deposits.
  • At depth, the felsic volcanics are well altered, the original host rock character locally obliterated by intense phengite alteration, a key alteration halo associated with VMS deposits (Figure 3).
  • Rock alteration and mineralogy, indicative of high temperature, further confirm an active hydrothermal system was present during deposition.
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