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Esgold Corp (2)
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Esgold releases ANT survey results for Montauban

2025-07-11 16:58 ET - News Release

Mr. Gordon Robb reports

ESGOLD UNLOCKS DISTRICT-SCALE DISCOVERY POTENTIAL AT MONTAUBAN WITH GEOLOGICAL STRUCTURES EXTENDING TO 1,200M

Esgold Corp. has released the results of its recent ambient noise tomography (ANT) survey operated by Caur Technologies at the Montauban gold-silver project in Quebec. The preliminary interpretation of this advanced seismic imaging has revealed multiple deep-seated geological structures, suggesting that the Montauban system may extend far beyond its historically mined zones -- opening the door to a potential district-scale mineral system.

Originally scoped to map subsurface structures to 400 metres, the ANT survey exceeded expectations -- imaging to depths of 1,200 metres and revealing a vertically extensive, laterally continuous geological system. These findings suggest that Montauban may represent a district-scale volcanogenic massive sulphide (VMS) environment, rather than a singular deposit, with structural and lithological features consistent with some of the most prolific mining camps globally.

Key highlights:

  • Imaging unveiled to depths of 1,200 metres: ANT survey has revealed deep-seated structural zones potentially hosting stacked mineralized lenses -- a breakthrough for exploration at Montauban.
  • New interpretation supports district-scale opportunity: Montauban may represent a clustered VMS system with structural repetition and geological similarities to world-class deposits like Sweden's Skellefte district.
  • North-central feeder zone emerges: Strong contrast between high-velocity basement in the north and structurally complex southern domains presents multiple potential discovery targets; while the southern area shows more structural complexity -- both priority areas for high-value targeting.
  • Historic assays plus VTEM plus ANT equals advanced model under way: The continuing 3-D geological model will integrate over 950 historic drill holes results, 2015 VTEM survey data and this new deep seismic imaging to identify next-generation discovery zones.

Andre Gauthier, PGeo, director of the company, added:

"We now believe Montauban may be far more than a single deposit -- it is emerging as a deep, district-scale system with possible structural and geological continuity," said Andre Gauthier, as a director of exploration. "These results may place Montauban into a new category of exploration potential. Where previous generations saw a series of shallow pods, we now see the signature of a vertically integrated mineral system -- potentially with stacked, repeating lenses akin to those in VMS system or Broken Hill-style districts. We're seeing signatures that resemble the structural architecture of globally significant systems, but we are still in the early stage of exploration."

A new lens on Montauban: from legacy mine to blue-sky discovery

Montauban has long been known for its shallow, high-grade production of gold, silver, lead and zinc, with over 2.6 million short tons historically mined. Yet until now, its deeper potential has remained locked beneath a century of fragmented data and under exploration.

The recently completed ANT survey -- a non-invasive geophysical technique using ambient seismic noise -- deployed 105 triaxial sensors across 10 square kilometres of the property, continuously recording data for 49 days. The resulting high-resolution 3-D shear-wave velocity model allows for unprecedented geological interpretation down to over 1,200-plus metres -- revealing a vertically continuous and structurally complex system that strongly supports a multilens, camp-scale model.

The imaging revealed:

  • Low-velocity zones near surface, corresponding to fractured, weathered and previously mined areas;
  • High-velocity basement rocks in the north-central region-suggesting compact, unfractured crystalline rock potentially hosting deeper feeder systems or stacked mineralized zones;
  • Strong structural contrast between northern and southern zones -- supporting the idea of multiple mineralized lenses rather than a single orebody.

The ANT data: depth, structure and untapped opportunity

The ANT results can be summarized by four key depth domains:

  • Zero to 300 metres: low-velocity, fractured rock consistent with historical shallow mining zones and weathered overburden;
  • 300 to 900 m: transitional zone with heterogeneous velocity - potential host for additional unmined mineralized horizons;
  • 900 to 1,200 m: a corridor of high-velocity rock, interpreted as crystalline basement or structurally competent feeder host -- particularly in the north-central zone;
  • Greater than 1,200 m: vertically extensive, pipe-like domains in the northern half suggest possible feeder conduits or high-grade remobilization corridors, while complex folding and low-velocity contrasts in the southern half suggest repeated mineralized lenses.

The ANT survey reaffirms that Montauban's mineral system remains open at depth -- both vertically and laterally -- and that multiple zones across the property remain completely untested.

"Montauban is no longer just a development story -- it's a discovery story in the making," said Gordon Robb, chief executive officer of Esgold. "This survey has fundamentally changed the way we understand this special deposit. The continuity, depth and scale of the structures we're seeing suggest that the original mine was just the tip of the iceberg. As we build toward production from the tailings, we're simultaneously unlocking the blue-sky potential beneath. This data confirms Montauban may be just the first chapter in a much larger district-scale opportunity, and we're excited to share that story with the world."

Why it matters to investors

  • District-scale upside: This is no longer a single-zone reprocessing story. Montauban is evolving into a modern exploration asset with potential scale comparable with known VMS camps.
  • Cash flow plus discovery: Tailings reprocessing still forms the backbone of the near-term production plan -- creating an ultrarare dual-track story where cash flow and discovery are pursued simultaneously.
  • Permits and construction in place: With permits secured and infrastructure installation under way, Esgold is positioned to capitalize on both operational and geological momentum.
  • Repeatable, scalable strategy: This platform model -- combining cash-flowing from tailings redevelopment with modern exploration -- is the blueprint for Esgold's long-term growth.

Caur Technologies successfully completed an ambient noise tomography (ANT) survey for Esgold over the Montauban mine site, located in Quebec's Capitale-Nationale region. The purpose of the survey was to image deep subsurface structures in support of gold exploration targeting volcanogenic massive sulfide (VMS) systems in a geologically complex area. The results provide valuable new insights into the geological framework of the site, offering a clearer understanding of the subsurface conditions that are critical for guiding exploration.

Despite extensive mining from 1910 to the 1970s targeting lead, zinc, silver and gold, the Montauban region remains underexplored at depth. Most geological data come from tailings and a few shallow boreholes, with virtually no deep-penetrating geophysical data. This hampers understanding of the extent, geometry and controls of mineralization. Ambient noise tomography (ANT) offers a non-invasive, cost-effective method to image deep crustal structures, highlighting velocity contrasts linked to lithological boundaries, alteration zones and structural traps. ANT can guide drilling and support robust geological models by revealing features beyond the reach of historic exploration -- unlocking untested targets and the region's deeper mineral potential.

The Montauban Group consists of quartzo-feldspathic gneiss, quartzite, marble, calcsilicates and metavolcanic units like pillowed tholeiitic metabasalt and lapilli metatuff. These formed in a shallow-submarine setting during a late andesitic-to-felsic volcanic cycle -- an environment favourable for volcanogenic massive sulphide (VMS) systems. The Montauban deposit is a gold-rich VMS system with stratiform to semi-massive lenses of Zn, Pb, Ag and Au, typically linked to sericite-chlorite alteration and localized along shear zones, fold hinges and lithological contacts.

The deposit's geometry reflects both syngenetic processes and structural reworking. Volcanic layers have been folded, faulted and transposed, while metamorphism altered mineral textures and paragenesis, complicating ore zone delineation. Though shallow mineralized zones have been identified, their deeper continuity remains unclear. The setting aligns with other reworked VMS systems in high-grade metamorphic terranes, suggesting significant untapped potential. Historically, over 2.6 million short tons of Zn-Ag-Au were extracted from multiple zones, including Tetreault-Anacon and Montauban, demonstrating strong vertical and lateral continuity.

Major mineral deposits in high-grade metamorphic terrains are uncommon, but notable examples include Broken Hill and Nova Bollinger in Australia, and Sweden's Skellefte and Bergslagen deposits.

Montauban shares some features with Broken Hill-particularly Pb-Zn-Ag mineralization and rare felsic metavolcanic rocks. However, Broken Hill is generally considered a SEDEX deposit in metasedimentary rocks and lacks significant gold. Nova Bollinger, a Ni-Cu sulphide deposit hosted in ultramafic intrusions, also differs in both host rocks and mineralization style.

Closer analogues are Sweden's Ravliden and Garpenberg deposits -- VMS systems formed in submarine volcanic settings and later metamorphosed during the 2.0 to 1.8 Ga Svecokarelian orogeny. These deposits and Montauban share key traits:

  • Deposit type: originally syngenetic VMS deposits later overprinted by orogenic processes;
  • Host rocks and metamorphism: occur in felsic-dominated metavolcanic sequences altered to amphibolite-granulite facies;
  • Mineralization: polymetallic (Pb-Zn-Ag plus or minus Au), lens-shaped and structurally complex;
  • Age: Ravliden is 2.0 to 1.8 Ga; Montauban is about 0.9 Ga;
  • Structural complexity: Montauban's folding, faulting and lens repetition resemble Skellefte's 3-D deformation patterns.

Unlike these better-known systems, Montauban has seen little modern exploration. Fragmented ownership, minimal deep drilling and limited geophysical work have hampered discovery of concealed mineralization. Yet the geological parallels strongly suggest untapped potential at depth.

Qualified person statement

The technical content of this release has been reviewed and approved by Andre Gauthier, PGeo, who is a director of Esgold and a qualified person under National Instrument 43-101 -- Standards of Disclosure for Mineral Projects (NI 43-101).

About Esgold Corp.

Esgold is a fully permitted, preproduction gold and silver mining company at the forefront of scalable clean mining and exploration innovation. With proven expertise in Quebec, the company is advancing its Montauban gold-silver project toward near-term production while unlocking long-term value through strategic redevelopment, modern discovery tools and sustainable resource recovery. Montauban, located 80 km west of Quebec City, represents a blueprint for cash-flow-generating legacy site redevelopment across North America.

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