Highlights 

  • The new hole REG-25-25 intersects 23.7 m of sulphide-specularite breccia comparable to past high-grade intervals. 
  • The mineralized breccia was intercepted 35 m up dip and along strike from REG-23-21. 
  • Four holes totaling 2476 m have been drilled so far in the 2025 follow-up program. 
  • The new Quartz-Feldspar Porphyry intersection could indicate additional mineralized pathways. 

Regency Silver Corp. (TSXV:RSMX) reports a meaningful geological development at its Dios Padre Project in Sonora, Mexico, with hole REG-25-25 intersecting 23.7 m of sulphide-specularite supported breccia. This breccia type hosts high-grade Au-Cu-Ag mineralization in past standout holes such as REG-22-01, REG-23-21, and REG-23-14. The new intercept lies approximately 35 m up dip and along strike to the southeast of REG-23-21, which previously returned 38 m of 7.36 g/t gold. 

The 2025 drill program, initiated on October 10, includes four completed holes totaling 2476 m. Visual comparisons show continuity of mineralized textures despite analytical results pending. Regency emphasizes caution in making grade assumptions but notes that geology, mineralogy, and alteration appear comparable to prior high-grade intervals reported in earlier campaigns. 

New QFP Discovery Enhances Geological Understanding 

A significant new development within REG-25-25 is the identification of mineralized shingle breccia occurring on both sides of an intersected Quartz-Feldspar Porphyry body. This geological feature is considered important, as porphyry intrusions at Dios Padre play a key role in creating brecciation and directing mineralizing fluids. 

The new QFP intersection suggests a possible continuation toward the historic Dios Padre silver mine and aligns with similar porphyry material noted at the bottom of REG-23-21. Regency Silver plans to follow this structural lead in upcoming drilling, including Hole 5, which aims to test continuity at shallower elevations. 

Additional holes drilled reveal extensions of sulphide mineralization even where high-sulphide breccia was not intercepted. REG-25-23 and REG-25-24 encountered notable sulphide zones in the projected target areas, indicating the broader mineral system remains active at depth and along strike. 

Quality Controls and Technical Oversight 

All core from the program underwent detailed logging, sampling, and chain-of-custody procedures. Samples were analyzed by ALS Global in Hermosillo, Mexico, using accredited methods for gold, silver, and base metals. Quality control materials, including blanks, duplicates, and certified standards, were inserted regularly to ensure analytical accuracy. 

Conclusion 

The intersection of sulphide-bearing breccia in REG-25-25, along with newly identified QFP bodies and widespread sulphide zones in multiple holes, provides meaningful evidence of continued mineralization across the Dios Padre system. With assays pending and further drilling underway, Regency Silver continues to advance its understanding of this expanding magmatic-hydrothermal environment.