Nicola Mining Aims to Identify Solid Drilling Targets on New Craigmont Through Targeted 3D-IP Surveys
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Editorial Team
Rundes Icon von GOLDINVEST - Das Investor-Magazin für Rohstoff-News und Rohstoff-Aktien
Editorial Team

New Porphyry Deposit Suspected

With targeted 3D-IP surveys on its New Craigmont copper project near Merritt, B.C., Nicola Mining Inc. (TSXV: NIM; FRA: HLIA) aims to test two previously identified targets in the upcoming exploration season to determine, on one hand, if the MARB-CAS zone could be a new version of the high-grade historical Craigmont Mine with skarn mineralization.

On the other hand, geologists suspect a potential new porphyry deposit in the so-called West Craigmont zone. Both target areas together cover 4.5 square kilometers (see Figure 1). They are part of Nicola’s total 10,913-hectare (>100 km²) license, which borders Canada’s largest copper mine, Teck Resources’ Highland Valley Copper. The IP survey is planned for late April/early May.

Map of the New Craigmont Project
Figure 1: Map of the New Craigmont project. The two areas to be investigated are shaded: The first zone is the MARB-CAS Zone, located immediately west of the Embayment Zone, while the second zone is the West Craigmont Zone, which hosts the WP MINFILE occurrence in the western part of New Craigmont.

Peter Espig, CEO of Nicola Mining Inc. commented: “Over the past two years, various modern exploration techniques have shown a significant correlation with older IP surveys and drilling. As the recently mapped mineralized outcrops align substantially with the observed anomalies, we are confident that the upcoming IP survey in the MARB-CAS and West Craigmont zones will yield solid drilling targets.”

In 2017 and 2018, Nicola flew 32.45 line kilometers of IP survey (marked in yellow in Figure 1). The survey results and subsequent exploration drilling showed a significant correlation between the IP data and high-grade copper intersections in the Embayment Zone (Figure 2).

Nicola Mining Abbildung 2 IP Aufladbarkeitsquerschnitt 200 m dick durch die Embayment Zone-GOLDINVEST
Figure 2: IP chargeability cross-section (200 m thick) through the Embayment Zone, showing a higher chargeability anomaly corresponding to high-grade copper intersections.

The goal of the IP survey is to find drilling targets west of the historical Craigmont Mine and the Embayment zones (Figure 1). Nicola’s geological team believes that the mineralized body has been offset by local faults and extends further to the west. The potential mineralization at the MARB-CAS anomaly is interpreted as analogous to the ore bodies of the historical Craigmont Mine and the exploration results in the Embayment Zone. The expected IP results are supported by copper mineralization observed and mapped in the MARB-CAS outcrops, both hosted in the Guichon quartz diorite.

The mineralization at CAS consists of magnetite breccia and magnetite-chalcopyrite mineralization associated with garnet-epidote-actinolite skarn. The MARB-CAS zone exhibits similar magnetite-associated geophysical features to the historical Craigmont Mine and the Embayment Zone (Figure 3).

Cross-sections Through the Magnetic Anomalies of CAS and MARB
Figure 3: Cross-sections through the magnetic anomalies of CAS and MARB, showing the target areas for IP and subsequent drilling in 2024.

The goal of the IP survey is to find a porphyry drilling target near the WP occurrence at West Craigmont. The 2022 ZTEM survey discovered a high-resistivity feature coinciding with a high-magnetism anomaly in the West Craigmont zone. The 2017 IP survey identified a chargeability anomaly to the southwest below the MARB 72 occurrence. The 2024 IP survey aims to determine if the ZTEM resistivity anomaly coincides with a chargeability anomaly, which would indicate a porphyry.

Nicola Mining Abbildung 4 Querschnitt durch WP-GOLDINVEST
Figure 4. Cross-section through WP, showing the ZTEM resistivity anomaly that possibly represents a felsic intrusion. The photos above the cross-section show malachite (copper-bearing green mineral) on the left side and a quartz vein with a halo of potassium feldspar (K) on the right side.
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