Churchill Confirms District-Scale Magmatic Intrusive Trend at Taylor Brook Nickel Project, Newfoundland & Labrador

Churchill Resources Inc.
Churchill Resources Inc.

In This Article:

Figure 1

MMT Resistivity Level Plans Show TB Magmatic Trend Widening at Depth
MMT Resistivity Level Plans Show TB Magmatic Trend Widening at Depth

Figure 2

Layden Section 2W and exploration model (from Barnes et al, 2018)
Layden Section 2W and exploration model (from Barnes et al, 2018)

Figure 3

Layden Area Detailed Drilling and MMT Plan
Layden Area Detailed Drilling and MMT Plan

TORONTO, Feb. 29, 2024 (GLOBE NEWSWIRE) -- Churchill Resources Inc. (“Churchill” or the “Company”) (TSXV: CRI) is pleased to announce that drilling and geophysical surveys completed this winter have confirmed a new, large, dynamic magmatic intrusive system (“TB Magmatic Trend”) that extends from the Layden Nickel Showing area southeasterly 13km to the Taylor Brook Gabbro Complex (“TGBC”) South Lobe. In particular:

  • CRI’s 2023 exploration confirms 13km TB Magmatic Trend with geophysics, soils, and diamond drilling

  • The TB Magmatic Trend extends from Layden Nickel Showing into the TBGC South Lobe

  • The TBGC South Lobe is of priority interest due to it’s intense gravity anomaly on the rifted continental margin; a type locale where nickel districts are commonly found

  • Drilling at Layden has successfully hit gabbroic intrusive rocks and sulphide-bearing breccias in all holes

  • Resistivity surveys are confirmed to have successfully mapped portions of the magmatic intrusive system

  • 2024 exploration is planned to blanket the 13km TB Magmatic Trend with conductivity surveys such that disseminated and massive sulphide targets can be detected

Bill Fisher, Chairman of the Board commented, “Churchill’s exploration team has had a successful year at Taylor Brook, and we’re incredibly excited by the definitive identification of the TB Magmatic Trend, and understanding it’s relationship to the Layden high-grade nickel as well as the rifted continental margin. Paul Sobie and his team have already shown there is a definitive age and rock-type relationship between Layden and the South Lobe of the TBGC and this trend or conduit has now been clearly mapped by our geophysical surveys. 2024 should be a big year for the project – we already have compelling drill targets at the LIT-1 and TBSL-1 nickel soil anomalies, and comprehensive follow-up along the trend should result in many more.”

The newly identified TB Magmatic Trend is characterized by low to very low resistivity responses in airborne Mobile Magnetotelluric (“MMT”) and ground Controlled Source Audio Magnetotelluric (“CSAMT”) surveys, which contrast with the highly resistive older gneissic country rock. Examinations of sectional and level plan resistivity data are showing a continuous dyke-like vertically oriented conduit that flares out into sill-like bodies at certain depths (Figure 1), including at Layden in the extreme north. Depth penetration was limited to ~600masl for the MMT survey due to the proximity of the power lines to the property which interfered with the lower frequency response.