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Emerita Intersects High Grade Copper-Gold Mineralization at El Cura; Mobilizes Second Rig to Accelerate El Cura Drill Program

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Emerita Intersects High Grade Copper-Gold Mineralization at El Cura; Mobilizes Second Rig to Accelerate El Cura Drill Program

 

 

 

 

 

Emerita Resources Corp. (TSX-V: EMO) (OTCQB: EMOTF) (FSE: LLJA) has intersected significant new mineralization in drilling at El Cura deposit area, part of Emerita’s wholly owned Iberian Belt West project (Please see Figure 1 below). IBW hosts three previously identified Volcanogenic Massive Sulfide deposits: La Infanta, La Romanera and El Cura. Results contained in this news release are from El Cura deposit area only. All three IBW deposits are open for expansion along strike and at depth.

  • Drill Hole EC013 intersected 10.6 m grading 1.7% copper, 0.95 g/t gold and 35.46 g/7 silver. This is the deepest and thickest intercept to date on El Cura area at approximately 300 m vertical depth.
  • Hole EC012 intersected 3.4 m grading 1.7% copper, 3.09 g/t gold and 49.3 g/t silver.
  • Hole EC008 intersected 2.6 meters grading 1.8% copper, 1.51 g/t gold and 73 g/t silver.
  • Mineralization has been intersected from near-surface to approximately 300 m vertical and appears to be getting thicker at depth. Follow up drilling in progress.
  • Intercepts are more than 600 m west of the historic El Cura mine workings.

 

 Figure 1: IBW claim block and locations of Romanera, El Cura and Infanta deposits.

 

Emerita Work at El Cura

 

Emerita has completed detailed geological mapping, as well as geophysical and geochemical surveys across the property, culminating in an initial scout drilling program (see news release dated January 31, 2024) in El Cura deposit area. This widely spaced core drilling intersected significant mineralization over approximately 400m x 300m (strike x dip-length), within a mineralized corridor of at least 600m of strike length. One of these initial drill holes, EC007, intersected 2.2m grading 2.9% Cu; 2.3% Pb; 4.6% Zn; 2.81 g/t Au and 82.5 g/t Ag in the western portion of the drilled area (Figure 2).

 

Figure 2: Plan map showing drill hole traces of the El Cura drilling, in red color holes in this NR.

 

An additional 2,300m in 8 diamond drill holes was subsequently budgeted to follow up this result. Approximately 220m of strike length was tested, focusing on the westernmost 200m of the 600m corridor, in the area of drill hole EC007. Massive to semi-massive sulfides were intersected down to 340m down hole (hole EC013) and remains open at depth and along strike to the west and east at this level (Figure 3 and 4; Table 1).

 

Figure 3: Geology map of El Cura area showing drill hole locations and location of historical mine workings.

 

Figure 4: Vertical long section projection showing drill hole pierce points (new holes in red).

 

Table 1: Assay results from recent drilling at El Cura

 

DDH Easting Northing Elevation Azimuth Dip Depth (m) FROM TO Width (m) Cu % Pb % Zn % Au g/t Ag g/t
EC008 649834 4171569 126 178 -48 300.5 283.8 286.4 2.6 1.8 1.2 1.9 1.51 74.00
EC009 649834 4171569 126 145 -45 344.4 319.7 320.9 1.2 0.8 0.8 1.4 1.08 41.00
EC010 649834 4171569 126 159 -55 455.3 Possible faulted Main Zone
EC011 649685 4171500 127 159 -45 368.7 243.3 245.2 1.9 0.3 0.3 0.8 0.31 10.42
EC012 649685 4171500 127 159 -58 437.2 262.8 266.2 3.4 1.7 0.8 2.8 3.09 49.03
incl.             264.3 266.2 1.9 3.1 1.5 5.0 5.47 86.95
EC013 649685 4171500 127 159 -70 422 328.8 339.4 10.6 1.7 0.6 1.0 0.95 35.46
incl.             333 337.1 4.1 3.1 1.1 1.6 1.76 62.29

 

Discussion

 

Results of the Company’s investigations to date at El Cura show a high-grade massive sulfide body, that strikes WNW-ESE, dips steeply to the north and plunges to the west characterized by high grades in copper and gold (EC012: 3.4m grading 1.7% Cu, 3.09 g/t Au, and EC013: 10.6m grading 1.7%, 0.95 g/t Au). The true thickness is approximately 75 to 85% of the intercept length. Recoveries are good, 98% average. Figure 5 below shows core photos of drillholes EC012 and EC013. Chalcopyrite, Galena and sphalerite can be appreciated as part of the massive sulfide mineralization.

 

Figure 5: core photos of drillholes EC012 and EC013 with abundant presence of Chalcopyrite, Sphalerite and Galena.

 

Further into the footwall there is a second mineralized zone which is highly siliceous and sericitic with disseminated sulfides up to 25% in volume characterized by moderate Zn and Pb grades (EC006: 2.8m grading 1.9% Zn, 0.9% Pb; EC010: 1.3m grading 2.1% Zn, 0.6% Pb).

 

The mineralization is hosted in a series of shales and volcaniclastic rocks, between two prominent ridges of felsic to intermediate subvolcanic intrusives or flows, lavas and agglomerates. This package has been overturned, folded and thrust to the south as is typical across the Iberian Pyrite Belt.

 

As defined thus far, El Cura appears to be higher grade to the west and thickening with depth. Conversely, it appears to shallow and thin to the east, presumably daylighting where it was worked by the Romans.   In the mid-20th century, underground exploration encountered massive sulfide of 1.5m thickness and 3% Cu 60m below surface in the same (Pinedo Vara). These workings are located approximately 600 meters east of the area presently being drilled. Additional drilling and interpretation has not yet been done to fully characterize the deposit to the east of these workings.

 

Drilling on section 9750E shows El Cura body located near to the contact between the upper shales and jaspers of the PTS Group and dacitic-rhyodacitic volcanics. The deposit dips approximately 75o to the north, with approximately 275m of down-dip extent defined thus far between EC007 and EC013. (Figure 6).

 

Figure 6: Interpretive geological cross section 9750E.

 

It is noteworthy that the EC013 intercept is the thickest to-date at El Cura, as well as the deepest. Hole EC014 is in-progress, designed to cut the deposit further down dip at a step out distance required for establishing an Indicated Mineral Resource drill spacing.

 

Joaquin Merino, Emerita’s President states “These six new drill holes have demonstrated the continuity of the El Cura massive sulfide body with high grades, especially in copper and gold. They transform El Cura into a very exciting target for the ongoing drill program. Importantly, this area is adjacent to potential planned underground infrastructure and close to the conceptual mill plant location and drilling is still shallow in this area”.

 

Next Steps

 

Given the strong results, additional drilling is being accelerated at El Cura. With the high-grade, near surface character of the El Cura mineralization, good potential exists to quickly outline significant tonnage near to envisioned development and processing facilities for the Romanera and Infanta deposits (Figure 5). Accordingly, a second rig was mobilized to El Cura and is expected to collar its first hole before month’s end. The two drills will then work to complete an additional 3,500m of drilling representing 13 to 15 additional holes, doubling the drill database for subsequent mineral resource estimation. The Company has the required drill platforms permitted to complete this program.

 

Figure 7: Conceptual underground infrastructure and surface facilities for IBW development. Note the central location of El Cura between Romanera and Infanta deposits and proximity to proposed haulageway.

 

Background

 

The IBW project and El Cura deposit is located at the westernmost extent of the Spanish Iberian Pyrite Belt near where the belt extends into Portugal. El Cura is mid-way between Emerita’s La Romanera and La Infanta Deposits. It lies along the southern of two mineral trends that have been located within the Company’s IBW exploration permit, along strike of the Infanta deposit 4km to the east. The Southern Trend continues westward from El Cura for at least another 2km as evidenced by old Roman-era workings and surface mapping and prospecting, parallel to the Northern Trend that hosts La Romanera deposit (Figure 1.)

 

Quality Assurance/Quality Control

 

Drilling at El Cura is HQ size and core is placed into core trays at the drill site and transported directly from the site to Emerita’s coreshack (15Km) from El Cura. Once the cores are received at Emerita’s coreshack they are photographed and geotechnical logging is performed. Geological, mineralogical and structural logging follows and mineralized zones are identified. The samples are marked every 1m or less, and respecting lithological contacts, with most of the samples 1.0m long. The zone immediately above and below the mineralized zones are also sampled. Core samples are sawed in half and half of the core is returned to the core tray for future reference. Once the core samples are cut, bagged and tagged, they are shipped to the ALS laboratory in Seville by Emerita personnel where sample preparation is done. In Seville, ALS performs the mechanical preparation of the samples and then the pulps are sent to ALS Ireland (ICP) and ALS Romania (fire assay). The analysis at ALS Lab corresponds to the ME-ICPore (19 elements) package, together with the Au-AA23 fire assay (Gold).

 

10% of the analyzed samples correspond to control samples (fine blanks, coarse blanks, high, medium and low grade standards). In addition, 10% of pulps are reanalyzed at a second independent certified laboratory (AGQ Lab Sevilla). When the analysis is completed, the certificates are received from the laboratory and the QA/QC protocol identifies any deviation or anomaly in the results and the entire batch is reassayed in such case. Once the data is approved by the QA/QC protocol assays are entered digitally directly into the database.

 

Qualified Person

 

Scientific and technical information in this news release has been reviewed and approved by Mr. Joaquin Merino, P.Geo., President of the Company and a Qualified Person as defined by NI 43-101.

 

About Emerita Resources Corp.

 

Emerita is a natural resource company engaged in the acquisition, exploration, and development of mineral properties in Europe, with a primary focus on exploring in Spain. The Company’s corporate office and technical team are based in Sevilla, Spain with an administrative office in Toronto, Canada.

 

Posted June 25, 2024

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New Break Resources Ltd. (CSE: NBRK) (OTCQB: NBRKF) (FSE: O91) has received results from the last four holes of a ten-hole, 1,996 metre summer drilling program in the Zavitz gold zone at the Company's 100% owned Moray gold project. In total, New Break has completed 5,372 metres of drilling in 32 drillholes in 2026. Moray is located 49 km southeast of Timmins, Ontario and 32 km northwest of the Young-Davidson gold mine operated by Alamos Gold Inc. Select results from the final four of ten holes drilled in the summer drilling program are presented below in Table 1, while drillhole collar locations are detailed in Table 2 in Appendix A. Table 1 – Moray Summer 2026 Final Drill Results Hole ID Length (m) From (m) To (m) Width (1) (m) Au Grade (2) (g/t) NBR-26-29 322.0 77.3 78.8 1.5 0.42 and 138.0 139.1 1.1 0.38 and 162.5 173.3 10.8 (3) 1.61 and 227.4 229.0 1.6 1.21 and 231.5 232.1 0.6 1.72 NBR-26-30 250.0 37.0 38.0 1.0 0.30 and 102.8 103.5 0.7 0.60 and 121.5 122.5 1.0 0.36 and 124.5 125.5 1.0 0.33 and 128.5 129.0 0.5 0.90 and 131.0 132.0 1.0 0.36 and 169.8 174.0 4.2 2.65 and 178.0 179.5 1.5 0.77 and 183.5 186.6 3.1 1.22 and 190.0 190.5 0.5 1.06 and 191.5 192.5 1.0 1.48 and 196.0 200.5 4.5 2.53 and 203.5 204.0 0.5 2.15 and 206.5 212.0 5.5 1.57 NBR-26-31 274.0 169.0 170.5 1.5 0.37 and 184.5 186.0 1.5 0.51 and 197.0 200.0 3.0 0.94 and 201.5 202.0 0.5 0.50 and 203.5 210.0 6.5 (3) 3.12 NBR-26-32 352.0 73.5 74.0 0.5 0.44 and 174.0 174.6 0.6 0.52 and 194.0 195.0 1.0 0.66 and 199.8 203.3 3.5 2.29 and 227.3 228.0 0.7 0.97 (1) Intervals are drill intersections and do not necessarily represent true widths. (2) All intervals are presented using a cut-off grade of 0.3 g/t Au and internal dilution of no more than 1.0 metres at grades less than 0.3 g/t Au and assays are not capped (see QA/QC Procedures). (3) Drill core photos shown in Appendix B. Figure 1 – Newly Reported Drillholes NBR-26-29, 30 Figure 2 – Newly Reported Drillholes NBR-26-30, 31, 32 Note: The bottom of NBR-26-30 deviated southeast and is represented in both sections. Figure 1: Section B-B1 incorporates drillholes NBR-26-06, 07, 08, 25, 26, 27, 28, 29 and part of 30. Gold mineralization extends southeast into the syenite as exhibited in NBR-26-29. NBR-26-30 is identified in both sections A-A1 and B-B1 as the drillhole was collared along section A-A1 but deviated southeast, intersecting gold mineralization in the mafic volcanics in section B-B1. Figure 2: A-A1 incorporates drillholes NBR-26-03, 04, 05, 23, 24, 30, 31 and 32. NBR-26-31 exhibits gold mineralization both within the syenite (at the contact) and within a "flow breccia" within the hematite altered mafic volcanic at the contact. NBR-26-32 is typified by blocky faulted ground with lamprophyre dykes and gold mineralization in the hematite altered mafic volcanics in a brecciated quartz vein with angular syenitic fragments. William Love, Chief Executive Officer of New Break commented, "Ongoing drilling this summer in the Zavitz gold zone continues to deliver significant gold values, with gold mineralization intercepted in every drillhole. As depicted in Figures 1 and 2, gold mineralization has been encountered predominantly within the mafic volcanics. Importantly, drillholes NR-26-29 and NR-26-32, the deepest drilled to date, demonstrate that gold mineralization extends into the syenite to the southeast at the contact with the mafic volcanics." He further noted, "The intrusive-mafic volcanic contact in the Zavitz gold zone has a distinctive magnetic high. This could be reflective of the higher proportion of iron in these mafic volcanics, which is associated with the higher gold values. This same magnetic and IP signature has been identified elsewhere in areas also believed to be along the intrusive-mafic volcanic contact. Drilling these never before tested targets with the goal of identifying gold mineralization similar to that encountered in the Zavitz zone represents the potential for significantly expanding the Moray gold discovery. There is also the belief that the Zavitz zone could represent the first of a series of stacked mineralized gold zones, which would point to the potential for a much larger gold system at depth. We plan to test this through deeper drilling directly into the Zavitz zone." About the Moray Gold Project The Moray property is located in the heart of the Ontario Abitibi greenstone belt, 49 km southeast of Timmins surrounded by a number of significant gold producing companies and existing mills (see Figure 3). The Young-Davidson gold mine operated by Alamos Gold Inc., with its 8,000 tonne per day mill is the closest and within a short trucking distance of approximately 45 km by road from Moray. The understanding of gold mineralization at Moray continues to evolve with each round of drilling. The occurrence of gold mineralization extending into the syenite to the southeast of the Zavitz zone and in the deepest drillholes is noteworthy given the presence of syenite-hosted mineralization at Young-Davidison. More recent examination of the drill core also suggests that the gold mineralization discovered to date may resemble an intrusion related style of deposit like Agnico Eagle's Upper Beaver gold deposit east of Kirkland Lake, as opposed to a structurally hosted gold system. Both Young-Davidson and Upper Beaver host multi-million ounce gold deposits. Figure 3 – Moray Location Map: Surrounding Gold Producers and Upper Beaver Gold Project Technical Content and Qualified Person The scientific and technical information contained in this news release has been reviewed and approved by Peter C. Hubacheck, P. Geo, consulting geologist to New Break, and an independent Qualified Person as defined by National Instrument 43-101. Mr. Hubacheck certifies that this news release fairly and accurately reflects the technical information and data presented. New Break conducts its exploration activities in accordance with CIM Best Practices Guidelines. QA/QC Procedures QA/QC procedures were executed to ensure all work is conducted in accordance with best practices. All drill core was sawn in half with one half of the core prepared for shipment and the other half retained for future verification. All core is under watch from the drill site to the core processing facility. Drill core is BQTK size and sample intervals range from 0.5 metres to 1.0 metres in length. Commercially prepared certified reference material ("CRM") standards and blanks were inserted with each shipment at a rate of 1 QAQC sample in every 12 core samples. Samples from New Break's 2026 Moray drilling program were analyzed at Activation Laboratories in Timmins, Ontario, which is ISO 17025 certified, by 30-gram fire assay with atomic absorption finish. Any sample assaying greater than 10.0 g/t Au was re-assayed with fire assay gravimetric analysis. Grade composite intervals over core lengths are calculated using a weighted average grade with a cut-off grade of 0.3 g/t Au. Up to 1.0 m of internal dilution (consecutive interval below cut-off grade) are included within specific geologic domains and alteration assemblages, except as otherwise noted. The composites are constrained geologically by metasomatic alteration processes sourcing from the Fiset syenite intrusion and contact mafic volcanic rocks. Elevated gold values are coincident with hematite, silica, sericite and pyrite mineralization within structurally prepared brecciated corridors flanking the intrusion. Intervals are not true widths and no top cutting has been applied to the higher gold values. About New Break Resources Ltd. New Break is a Canadian mineral exploration company focused on its Moray gold project located 49 km southeast of Timmins, Ontario, in a well-established mining camp within proximity to existing infrastructure, and 32 km northwest of the Young-Davidson gold mine, operated by Alamos Gold Inc. Shareholders are also leveraged to exploration success in Nunavut, Canada, through New Break's 20% carried interest in the Sundog gold project and ownership of 6.0 million shares of Guardian Exploration Inc. (TSXV: GX). The Company is supported by a highly experienced team of mining professionals. Appendix A – Drillhole Data and Locations Table 2 – Moray Summer 2026 Drillhole Collar Locations Hole ID Length (m) UTM Easting UTM Northing UTM Elevation Azimuth (degrees) Dip (degrees) NBR-26-29 322.0 492703 5320285 363 220 -70 NBR-26-30 250.0 492708 5320329 363 220 -47 NBR-26-31 274.0 492708 5320329 363 220 -60 NBR-26-32 352.0 492708 5320329 363 220 -70 Total 1,198.0 Coordinates are reported in UTM Zone 17 North, with units in metres. Figure 4 – Zavitz Gold Zone – Surface Traces of 2025 and 2026 Drillholes. All of the drilling at Moray has been completed by Enviro North Exploration Inc. out of Sturgeon Falls, Ontario. Drilling in the Zavitz gold zone is shown in figure 4, with the 1,996 metres in 10 holes drilled this summer depicted in red, the 2,807 metres in 20 holes drilled from January to April 2026 shown in blue and the 1,817 metres in 8 holes drilled in 2025 shown in black. In total, 6,620 metres in 38 drillholes have been completed in the Zavitz gold zone, while New Break has completed a total of 5,372 metres in 32 drillholes of our planned 2026, 10,000 metre drilling program. Appendix B – Drill Core Photos From NBR-26-29 and NBR-26-31

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