Turmalina Expands Mineralization at Veta Rica and Discovers New Mineralized Zones

In This Article:

Turmalina Metals Corp.
Turmalina Metals Corp.

Figure 1

Regional view northwest showing the block of properties controlled by Turmalina Metals with the drill target locations drilled in this campaign and the previously drilled San Francisco Breccia.
Regional view northwest showing the block of properties controlled by Turmalina Metals with the drill target locations drilled in this campaign and the previously drilled San Francisco Breccia.

Figure 2

Geologic map showing veins, breccias and gold in rock chip samples across the Veta Rica, Destino and Machete target areas.    Mapping and sampling have identified multiple mineralised veins at Veta Rica, Machete and Destino, and mapping is currently underway to define a potential new target in the top right of the map (21 g/t Au).
Geologic map showing veins, breccias and gold in rock chip samples across the Veta Rica, Destino and Machete target areas. Mapping and sampling have identified multiple mineralised veins at Veta Rica, Machete and Destino, and mapping is currently underway to define a potential new target in the top right of the map (21 g/t Au).

Figure 3

Veta Rica Surface map and sections showing drill holes and distribution of rock chip sampling of the Veta Rica vein.  Sampling 300 m west of the drill pads has returned grades of up to 27 g/t Au, while samples 700 m west of the drilling has returned grades of up to 2.7 g/t Au.
Veta Rica Surface map and sections showing drill holes and distribution of rock chip sampling of the Veta Rica vein. Sampling 300 m west of the drill pads has returned grades of up to 27 g/t Au, while samples 700 m west of the drilling has returned grades of up to 2.7 g/t Au.

Figure 4

Drone photo looking northwest showing 700 m strike length of Veta Rica, select surface rock chip samples and established drill pads. The Veta Rica vein remains open to both the west and, in the foreground, to the east where it passes under shallow cover.
Drone photo looking northwest showing 700 m strike length of Veta Rica, select surface rock chip samples and established drill pads. The Veta Rica vein remains open to both the west and, in the foreground, to the east where it passes under shallow cover.

Figure 5

Photo of core in hole SFDH-078 and hand sample from outcrop at the extension along strike of Veta Rica: Brecciated crystalline quartz surrounded by intense sericite alteration with iron oxide and jarosite, formed after weathering of sulphides.
Photo of core in hole SFDH-078 and hand sample from outcrop at the extension along strike of Veta Rica: Brecciated crystalline quartz surrounded by intense sericite alteration with iron oxide and jarosite, formed after weathering of sulphides.

Figure 6

Examples of high-grade gold mineralisation in core samples and from an outcrop along strike from drilling at Veta Rica. Mineralisation is hosted in crystalline quartz (commonly brecciated) with intense sericite alteration and hematite-goethite-jarosite, formed by the weathering of sulphides.
Examples of high-grade gold mineralisation in core samples and from an outcrop along strike from drilling at Veta Rica. Mineralisation is hosted in crystalline quartz (commonly brecciated) with intense sericite alteration and hematite-goethite-jarosite, formed by the weathering of sulphides.

Figure 7

Plan map of the newly discovered Destino vein and breccia system showing distribution of gold grades in rock chip samples that returned up to 22.2 g/t Au. Gold mineralisation is hosted within both epithermal quartz veins and adjacent quartz-tourmaline breccias.
Plan map of the newly discovered Destino vein and breccia system showing distribution of gold grades in rock chip samples that returned up to 22.2 g/t Au. Gold mineralisation is hosted within both epithermal quartz veins and adjacent quartz-tourmaline breccias.

Figure 8

Photos of an epithermal vein at Destino. Mineralization is hosted in epithermal quart veins (locally banded) and within intensely brecciated and sericite-altered granodiorite and diorite that hosted abundant hematite-goethite-jarosite veinlets.
Photos of an epithermal vein at Destino. Mineralization is hosted in epithermal quart veins (locally banded) and within intensely brecciated and sericite-altered granodiorite and diorite that hosted abundant hematite-goethite-jarosite veinlets.

Figure 9

Machete epithermal vein zone. The veins and gold mineralization are hosted in strongly sericite-altered granodiorite (a), with quartz veinlets (b) and portions brecciated with green/grey silica and iron oxides and jarosite. Float in the area includes samples of finely banded silica and iron oxide (d) and breccia with matrix of crystalline quartz (comb texture) with fragments of finally banded silica and iron oxides after sulphides (e), both textures typical of epithermal veins.
Machete epithermal vein zone. The veins and gold mineralization are hosted in strongly sericite-altered granodiorite (a), with quartz veinlets (b) and portions brecciated with green/grey silica and iron oxides and jarosite. Float in the area includes samples of finely banded silica and iron oxide (d) and breccia with matrix of crystalline quartz (comb texture) with fragments of finally banded silica and iron oxides after sulphides (e), both textures typical of epithermal veins.

VANCOUVER, British Columbia, Nov. 15, 2023 (GLOBE NEWSWIRE) -- Turmalina Metals Corp. (“Turmalina”, or the “Company”; TBX-TSXV, TBXXF-OTCQX, 3RI-FSE) is pleased to announce results from continued surface work at the Company’s 403 km2 San Francisco project located in the prolific mining province of San Juan, Argentina (the “Project” or “San Francisco”). Following the recent discovery of the high-grade epithermal gold vein system at Veta Rica (see announcement dated October 10th, 2023) field work has focused on mapping and sampling the surrounding area. This surface work has discovered multiple mineralized veins in the immediate vicinity of Veta Rica and has also discovered two new zones of similar epithermal mineralization located approximately two and four kilometres northwest of Veta Rica: the Machete and Destino systems respectively.

Highlights of Veta Rica Target Area

  • Recent mapping has traced the Veta Rica epithermal vein for over 700 m on surface with surface widths of 1 to 6 m: Surface gold assays are typically between 0.9 and 2.7 g/t Au but with higher grade zones of up to 56.6 g/t Au.

  • This mapping has also identified multiple mineralized veins adjacent to, and parallel with, the Veta Rica vein (Figures 2, 3 & 4) with similar average grades (typically 0.45 to 4 g/t Au). Detailed sampling is underway to identify potential high-grade zones in these newly discovered veins.

  • Recently announced drill holes at Veta Rica returned:

    • 4.4 m @ 6.4 g/t Au; SFDH-078 from 36.6 m.

      • Including 0.5 m @ 28.6 g/t Au from 36.6 m.

      • And 0.45 m @ 14.12 g/t Au from 38.85 m.

    • 8.75 m @ 3.5 g/t Au; SFDH-079 from 42 m.

      • Including 6.0 m @ 4.6 g/t Au from 42 m.

      • Including 1.18 m @ 17.9 g/t Au from 42 m.

Highlights of Destino Target Area

  • A new system with at least four parallel epithermal quartz veins, and two adjacent breccias, located 3 km northwest of Veta Rica (Figure 2, 7, 8 & 9).

  • Initial sampling (56 samples) of the veins, each with over 200 m of strike length, returned similar gold grades to Veta Rica, with 10 samples over 1 g/t Au, up to a maximum of 6.1 g/t Au (Figure 7).

  • In the southern portion of the Destino target area, 34 samples taken from a 100 by 130 m breccia pipe (the Tiki-Tiki breccia) returned four samples over 1 g/t, up to a maximum of 22 g/t Au, 227 g/t Ag and 0.9% Pb.

Highlights of Machete Vein zone

  • Located between Veta Rica and Destino, 2.7 km northwest of Veta Rica drilling, 3 rock chip samples taken from the Machete epithermal quartz vein returned grades of 1.1 to 2.7 g/t Au and 28 to 170 g/t Ag. Follow up sampling is underway (Figures 2 & 9).