.
Regency Silver (OTCQB: RSMXD) reports that drill hole REG-25-25 intersected 23.7 m of sulphide‑specularite supported breccia, a lithology comparable to previously reported high‑grade breccias. Historical comparative intervals include REG-23-21: 38 m @ 7.36 g/t Au, REG-22-01: 35.8 m @ 6.84 g/t Au, 0.88 % Cu, 21.82 g/t Ag, and REG-23-14: 29.4 m @ 6.32 g/t Au. Four 2025 holes (2,476 m) have been completed; assay results for the 2025 program are pending.
A new quartz‑feldspar porphyry (QFP) was intersected within REG-25-25 on both sides of the breccia. The discovery will be followed up toward the historic Dios Padre silver mine.
Positive
- REG-25-25 intersected 23.7 m of sulphide breccia
- Historical intercepts: 38 m @ 7.36 g/t Au
- Historical intercepts: 35.8 m @ 6.84 g/t Au, 0.88 % Cu
- New QFP intersection potentially vectors mineralization
Negative
- No assays yet for the 2025 drill program – results pending
- Several 2025 holes did not hit high‑sulphide breccia
- REG-25-24 mineralization terminated by a fault at ~515 m depth
Vancouver, British Columbia – Regency Silver Corp. (TSXV: RSMX) (OTCQB: RSMXD) announced that follow‑up drill hole REG‑25‑25 intersected 23.7 m of sulphide‑specularite breccia (Figure 1). The breccia is analogous to that hosting high‑grade Au‑Cu‑Ag mineralization in historic holes REG‑22‑01, REG‑23‑21 and REG‑23‑14. The intercept lies approximately 35 m up‑dip and along strike to the southeast of hole REG‑23‑21, which yielded 38 m of 7.36 g/t Au. Hole REG‑22‑01 returned 35.8 m of 6.84 g/t Au, 0.88 % Cu and 21.82 g/t Ag, while REG‑23‑14 intersected 29.4 m of 6.32 g/t Au.
The 2025 follow‑up program began on 10 October 2025. To date, four holes totalling 2,476 m have been completed, including an extension of a vertical hole drilled in 2012. Hole locations and trajectories are illustrated on the plan view (Figure 2) and the 3D long‑section (Figure 3). The next hole, designated REG‑25‑05, will test the continuity of the breccia at shallower depths up‑dip toward the historic Dios Padre silver mine.
Preliminary visual inspection of REG‑25‑25 shows robust alteration, abundant sulphide mineralization and mineral species consistent with the historic high‑grade intervals. Although assay results are still pending, the geological signature strongly suggests comparable ore‑grade potential. For reference, detailed assay data for the historic intercepts can be found in company releases dated 23 February 2023 and 2 November 2023.
A key development in REG‑25‑25 is the discovery of a quartz‑feldspar porphyry (QFP) that brackets the mineralized breccia on both sides. QFP bodies are recognized as the primary drivers of brecciation and fluid flow in the Dios Padre system, creating pathways for sulfide deposition. The newly identified QFP appears to extend toward the bottom of the mineralized zone encountered in REG‑23‑21, offering a promising vector for additional Au‑Cu‑Ag zones.
Summary of additional holes drilled
- DP‑01‑2012‑EXT – Extension below 300 m of a historic hole that stopped short of the projected breccia. Broad zones of disseminated and vein‑hosted sulphide were intersected shortly after 300 m, confirming extension of the mineralized system to the northwest. No high‑sulphide breccia encountered; results pending.
- REG‑25‑23 – Targeted a deeper southeast extension of the breccia. Intersected 120 m (≈550‑670 m depth) of disseminated and locally vein‑hosted sulphides consistent with the projected zone, but no high‑sulphide breccia; results pending.
- REG‑25‑24 – Targeted a shallower southeast extension. Intersected 114 m (≈400‑514 m) of new disseminated sulphide mineralization, which abruptly terminates at a fault near 515 m depth; no significant mineralization beyond the fault; results pending.
Table 1: Drill‑hole coordinates and orientation
| Hole ID | Easting | Northing | Elevation | Depth | Azimuth (°) | Dip (°) |
|---|---|---|---|---|---|---|
| DP‑01‑2012‑EXT | 690349 | 3150867 | 1282 | 543 | 0 | -90 |
| REG‑25‑23 | 690750 | 3150880 | 1395 | 740 | 228 | -64.1 |
| REG‑25‑24 | 690750 | 3150880 | 1395 | 742.3 | 227.8 | -60 |
| REG‑25‑25 | 690750 | 3150880 | 1395 | 742 | 233 | -57.7 |
* The hole orientations were adjusted in this program to intersect the mineralized breccia at true width now that its geometry is better constrained. Topographic constraints required higher collar elevations, resulting in longer drill lengths. True‑thickness intersected is estimated at 70‑100 %.
Technical Information
The technical content of this release has been reviewed and approved by Michael Tucker, P. Geo, a Qualified Person under NI 43‑101. Mr. Tucker is also a director of Regency Silver.
Quality Assurance / Quality Control
Core samples were logged, split, labelled and bagged for assay. Quality‑control samples—including blanks, duplicates and standards—were inserted at regular intervals. All shipments were performed under chain‑of‑custody procedures.
Samples were sent to ALS Global’s laboratory in Hermosillo, Mexico. Gold assays were performed by fire‑assay with atomic‑absorption finish (Au‑AA23) and gravimetric finish (Au‑GRA21) for values above 10 ppm. Silver and base‑metal assays were conducted by multi‑element ICP‑AES (ME‑ICP61m) with appropriate digestion protocols. ALS Global holds ISO 9001 and ISO/IEC 17025 certifications; all QC results met acceptance criteria.
About Regency Silver Corp.
Regency Silver Corp. is a Canadian resource company focused on the exploration of high‑grade gold, copper and silver projects in Mexico. Its flagship property, the Dios Padre project in Sonora, hosts a large magmatic‑hydrothermal system that widens at depth. Historic drill results have demonstrated significant grades, including 38 m @ 7.36 g/t Au (REG‑23‑21), 35.8 m @ 6.84 g/t Au, 0.88 % Cu, 21.8 g/t Ag (REG‑22‑01) and 29.4 m @ 6.32 g/t Au (REG‑23‑14).
Neither the TSX Venture Exchange nor its Regulation Services Provider accepts responsibility for the adequacy or accuracy of this release.
Cautionary Note Regarding Forward‑Looking Statements: This release contains forward‑looking statements that involve known and unknown risks, including the need for additional financing, regulatory approvals and the inherent uncertainties of mineral exploration. Results may differ materially from expectations. The company does not undertake to update any forward‑looking statements, except as required by applicable securities laws.

Figure 1: Photographs of the sulphide‑specularite breccia that hosts Au‑Cu‑Ag mineralization at Dios Padre.

Figure 2: Plan view of current and historic drill‑hole locations. The projected breccia surface is shown in red.

Figure 3: 3D long‑section illustrating the breccia zone, drill‑hole trajectories, block model and historic mine workings.
FAQ
What did Regency Silver announce on December 8, 2025?
Regency Silver reported that drill hole REG‑25‑25 intersected 23.7 m of sulphide breccia and discovered a new quartz‑feldspar porphyry; assay results for the 2025 program are still pending.
How does the geology of REG‑25‑25 compare with earlier holes?
Geologically, REG‑25‑25 is comparable to high‑grade intervals such as REG‑23‑21 (38 m @ 7.36 g/t Au), but assay data for the new intercept are not yet available.
Which historic drill results were cited for comparison?
The release references REG‑23‑21 (38 m @ 7.36 g/t Au), REG‑22‑01 (35.8 m @ 6.84 g/t Au, 0.88 % Cu, 21.82 g/t Ag) and REG‑23‑14 (29.4 m @ 6.32 g/t Au).
What is the status of the 2025 assay results?
Assay results for all 2025 drill holes remain pending.
Why is the new QFP intersection important?
Quartz‑feldspar porphyries act as brecciation sources and fluid conduits. The newly identified QFP could help vector exploration toward additional Au‑Cu‑Ag mineralization zones.
Which 2025 holes did not intersect high‑sulphide breccia?
Holes REG‑25‑23 and REG‑25‑24 intersected disseminated sulphides but did not encounter the high‑sulphide breccia; assay results are awaited.
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