VANCOUVER, BC, Aug. 4, 2026 /CNW/ -- Targa Exploration Corp. (CSE: TEX) (FRA: V6Y) (OTCQB: TRGEF) ("Targa" or the "Company") today announced additional assays results from the Company's drill program at the El Zanjon gold-silver project in Santa Cruz, Argentina (the "Project"). Assays results from holes EZD0003 through EZD0008 are reported below.
Maiden drill program at El Zanjon now complete. A total 2,475m was drilled in 10 holes testing three target areas (NE-AOI, NW-AOI, EZ Fault)
Narrow zones of anomalous silver values observed in EZD0003-0005, -0007 and -0008
Thick intervals of favorable quartz-feldspar lapilli tuff encountered in EZD0007, -0008
Final assay results for the last two holes (EZD0009 and EZD0010) expected in the next 3weeks
"This first pass drill program has produced a significant amount of data and a new understanding of the underlying geology at El Zanjon where there is only a single outcrop in over 57,000 hectares," commented Targa CEO, Cameron Tymstra. "We've only just gotten started at El Zanjon with this program andthis new information will help considerably in formulating our targeting methods and exploration strategy for future phases of work at El Zanjon as we continue to narrow our search for epithermal systems on the project. The 2,475m we just completed also puts us well ahead of our earn-in obligationsfor 2026. While we wait on assays for the last two holes and begin a detailed analysis of the captured data, we are finalizing plans for our Phase 2 Opinaca drill program, details of which are expected to be released in the coming days. I am very excited about this upcoming drill program at Opinaca, where last year we hit gold in seven out of eight drill holes across a strike of 4km. "
Ryan Weston, VP Exploration with Targa states: "With the completion of our maiden drill program at El Zanjon come several new geological insights. Based on the drilled lithologies between the NE-AOI and NW-AOI, we believe the volcanic stratigraphy to be shallowly dipping to the southeast, with intermediate volcanic tuffs and flows overlying a thick felsic ignimbrite sequence. This is similar to what we know about the Chon Aike volcanic formation in the Cerro Vanguardia low-sulphidation epithermal vein field 30km along strike to the northwest of El Zanjon.
While assays results to date have not yielded significant precious metal values, the wider intersection of anomalous silver values within the altered felsic ignimbrite unit in EZD0007 is encouraging and may be an early indication of a hydrothermal centre of mass for the property. Over the coming weeks we will fully evaluate all geochemical, geological and geophysical data to inform our next phase of work for the El Zanjon project."
Hole EZD0003 through EZD0008 Results
Holes EZD0003 and 0004 were drilled on a north oriented fence (Table1) in area NE-AOI targeting east trending magnetic lineaments coincident with a large multi-element soil anomaly (Figures1,2). Both holes intersected Jurassic basement volcanic rock at 60m depth below the Tertiary cover sequence. Basement volcanic units consist of strongly clay altered intermediate lithic volcanic tuff followed by a pervasively oxidized and clay altered amygdular andesite unit below between 145m and 195m depth and continuing to end of hole. Assay highlights are limited to narrow (<3m) intervals of anomalous silver (2-5ppm Ag) and weakly anomalous gold (10-70ppb Au).
Hole EZD0005 was a scissor hole drilled south on the same section as holes EZD0001 and 0002, in area NE-AOI targeting a southeast trending magnetic lineament coincident with a large multi-element soil anomaly. Basement volcanic units beginning at 60m depth are dominated by the same oxidized and coarsely amygdular andesite unit observed in holes EZD0001 and -0002, with amygdules commonly filled by white kaolinitic clay. Assay highlights are limited to a single 1m interval of 13.97ppm Ag in Tertiary marine sediment at the Tertiary-Jurassic contact, and a single narrow (<1m) interval of anomalous silver (2ppm Ag) in basement volcanics. Gold values were all below detection (<10ppb Au).
Hole EZD0006 was drilled 1.5km to the southeast of holes EZD0001, -0002 and -0005, and targeted the same magnetic lineament within a multi-element soil anomaly. Basement volcanic rocks beginning at 69m depth consists entirely of the strongly clay altered intermediate lithic volcanic tuff unit observed at the top of holes EZD0003 and -0004. On the basis of these pierce points into this unit, basement stratigraphy in the NE-AOI is interpreted to be dipping shallowly to the southeast, in line with the dip of the Chon Aike formation at Cerro Vanguardia. Hole EZD0006 did not return any significant assays.
Hole EZD0007 was drilled 2.9km to the west of holes EZD0001, -0002 and -0005, in NE-AOI, targeting the interpreted intersection of east-west and southeast trending magnetic lineaments coincident with a multi-element soil anomaly. Basement volcanic rocks between 56-145m depth consists of an intermediate sequence of fine ash-tuff, coarse andesite breccia and lithic tuff, all strongly clay altered and locally hematized. From 145-200m (end of hole) the hole encountered a felsic sequence dominated by quartz-feldspar porphyritic lapilli tuff and lesser finely laminated felsic ash tuff. Alteration in this lower felsic unit appears intense and varies from clay-dominated (argillic) to chlorite-dominated (propylitic), ending with patchy pervasive limonite-hematite alteration. Elevated silver values, including up to 2.43ppm Ag over 6.40m, were encountered between 168.70-180.0m in this lower felsic unit. All gold values returned below detection limit levels.
Hole EZD0008, drilled in the NW-AOI, targeted the interpreted intersection of east-east and southeast trending magnetic lineaments coincident with a 1.5km long multi-element soil anomaly (Figure3). Basement volcanic rock was encountered at 70m depth and consists entirely of quartz-feldspar porphyritic lapilli tuff. This same unit is exposed in outcrop 4.1km to the southwest and is interpreted to be a welded ignimbrite on the basis of flattened lapilli, lack of porosity and elevated hardness (Figure4). Alteration in EZD0008 is limited to clay and limonite staining (interpreted to be weathering related) above 110m depth, below which the unit appears quite fresh. Assay highlights in this hole are limited to two narrow (<3m) intervals of anomalous silver (2-3ppm Ag) and several gold values at detection level (10ppb Au).
Table 1: Collar details for EZD0003 through EZD0008
Hole
Easting*
Northing*
Azimuth
Dip
Length
EZD0003
582,320 mE
4,603,240 mN
0º
-50º
203.0m
EZD0004
582,320 mE
4,602,140 mN
0º
-50º
221.0m
EZD0005
581,280 mE
4,603,208 mN
180º
-50º
221.0m
EZD0006
582,640 mE
4,602,444 mN
180º
-50º
277.0m
EZD0007
578,330 mE
4,603,036 mN
0º
-55º
200.0m
EZD0008
562,960 mE
4,604,460 mN
0º
-50º
200.0m
*WGS 84 Zone 19S
Table 2: Assay highlights for EZD0003 through EZD0008
Hole
From (m)
To (m)
Width (m)
Est. true width (m)
Ag (ppm)
EZD0003
55.73
56.50
0.77
unknown
5.35
EZD0003
142.00
143.35
1.35
unknown
2.06
EZD0003
176.00
177.00
1.00
unknown
2.28
EZD0003
179.25
180.00
0.75
unknown
3.21
EZD0004
60.00
60.90
0.90
unknown
2.34
EZD0004
64.00
66.00
2.00
unknown
2.11
EZD0004
204.35
204.95
0.60
unknown
2.08
EZD0005
59.00
60.00
1.00
unknown
13.97
EZD0005
88.30
89.00
0.70
unknown
2.15
EZD0006
NSV
EZD0007
67.00
67.85
0.85
unknown
2.06
EZD0007
162.85
163.33
0.48
unknown
2.84
EZD0007
168.70
175.10
6.40
unknown
2.43
EZD0007
179.00
179.50
0.50
unknown
2.88
EZD0007
179.50
180.00
0.50
unknown
3.18
EZD0008
71.00
72.00
1.00
unknown
2.16
EZD0008
91.00
92.00
1.00
unknown
2.35
EZD0008
107.30
108.00
0.70
unknown
3.3
EZD0008
108.00
108.65
0.65
unknown
2.8
QAQC program
Drill core for the El Zanjon project was transported daily from the drill to the logging facility where it was logged, photographed, and split by diamond saw prior to being sampled. Internal blanks and certified reference materials were inserted into the sample stream at regular intervals as part of Targa's internal QAQC program. Groups of samples were then placed in large bags and transported from the project site to Alex Stewart International (ASI), an ISO 9001 and ISO 17025 certified analytical laboratory, in San Julian.
Sample preparation at ASI consists of drying, crushing and pulverizing to <106µm (prep code P1 and P5). Following preparation, pulp samples were then shipped to ASI in Perito Moreno for fire-assay gold and silver analysis (code Au4-30 and Ag4A-30), and to ASI in Mendoza for 39-element multi-acid ICP-OES (code ICP-MA 39) to determine trace element composition.
All results presented passed the QA/QC screening at the lab, as well as Targa's internal QAQC program within acceptable limits.
Technical Disclosure
The disclosure of scientific and technical information contained in this news release has been reviewed and approved by Ryan Weston, P.Geo., VP of Exploration of Targa, who is a "qualified person" within the meaning of National Instrument 43 -101- Standards of Disclosure for Mineral Projects. Mr. Weston is responsible for the technical content of this news release and is not independent of the Company.
Targa Exploration Corp. (CSE: TEX | FRA: V6Y | OTCQB: TRGEF) is a Canadian exploration company engaged in the acquisition, exploration, and development of gold mineral properties with headquarters in Vancouver, British Columbia. The Company's focus is on early-stage projects in premier mining jurisdictions with strong potential for making Tier 1 grass roots precious metals discoveries. Targa's flagship asset is its Opinaca gold project in Quebec where wide-spread gold mineralization was recently discovered during a maiden drill campaign in 2025. The Company has also recently acquired options to earn up to 80% equity interests in the Venidero and El Zanjon gold-silver projects in Santa Cruz, Argentina and is actively drilling at El Zanjon.
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