Mr. Zachary Kotowych reports

TROUBADOUR RESOURCES INTERCEPTS TARGET MINERALIZATION NEAR SURFACE DURING PHASE 1 OF THE MULTI-PHASE DRILL PROGRAM AT SENNEVILLE GOLD-SILVER-COPPER PROPERTY

Troubadour Resources Inc. has intercepted target mineralization during phase 1 of the multiphase drill program at its Senneville gold-silver-copper property.

Phase 1 drill campaign highlights:

• The completed phase 1 drilling campaign was focused on the Gustav Cere showing based on the data obtained from the recently completed induced polarization (IP) surveys (see press release dated Jan. 18, 2026).
• The high-grade gold mineralization seen at the property is hosted in quartz-carbonate-tourmaline veins along both the footwall and the hangingwall of the Senneville komatiite that bear many similarities to the gold-bearing veins of the neighbouring Novador deposits.
• Seven drill holes totalling approximately 1,000 metres were drilled focusing on near-surface targets.

Target mineralization intervals were intercepted along all seven phase 1 drilling campaign drill holes.

Drill holes SV-25-002, SV-25-007, SV-25-006 and SV-25-003 intercepted the longest cumulative mineralization intervals:

• SV-25-002: 57.8 metres of target mineralization was intercepted beginning at 20.14 metres downhole, with multiple intervals over four metres in width up to 19.35 metres;
• SV-25-007: 50.6 metres of target mineralization was intercepted beginning at 2.65 metres downhole, with multiple intervals over five metres in width up to 21.5 metres;
• SV-25-006: 44.6 metres of target mineralization was intercepted beginning at 15.01 metres downhole, with multiple intervals over three metres in width up to 7.4 metres;
• SV-25-003: 39 metres of target mineralization was intercepted beginning at 2.65 metres downhole, with multiple intervals over five metres in width up to 13 metres.

The mineralization is mainly associated with quartz carbonate veins and veinlets in forms of disseminated sulphides, stringers, clusters and fracture filling within sheared and deformed lithological terrains. The main mineralization hosting lithology is sheared and deformed volcanics dominantly in the form of mafic volcanics (basalt) and less intermediate sequences, including andesite and volcanosediments.

The mineralized sections of SV-25-002 dominantly including pyrite and less pyrrhotite with trace magnetite in different forms of disseminated, cluster, stringer and fracture filling are hosted within the sequence of sheared and partially extensionally deformed mafic to intermediate volcanic and less intermediate tuff rock formations associated with quartz-carbonate vein and veinlet system and the main alteration products of chloritization, carbonatization, and less biotitization and silicification.

The mineralized sections of SV-25-007 dominantly including pyrite and less pyrrhotite in different forms of disseminated, cluster, stringer and fracture filling are hosted within the sequence of sheared and partially extensionally deformed mafic volcanics and less intermediate intrusions and volcanoclastic rock formations associated with quartz-carbonate vein and veinlet system and the main alteration products of chloritization, carbonatization, and less silicification and biotitization.

The mineralized sections of SV-25-006 dominantly including pyrite and less pyrrhotite with some trace magnetite in different forms of disseminated, cluster, stringer, semi-massive and fracture filling are hosted within the sequence of sheared and partially extensionally deformed mafic volcanic and less intermediate volcanics, volcanosediments and intrusion rock formations associated with quartz-carbonate vein and veinlet system and also main alteration products of chloritization, carbonatization, biotitization, and less silicification and seriticization.

The mineralized sections of SV-25-003 dominantly including pyrite and less pyrrhotite in different forms of disseminated, cluster, stringer and fracture filling are hosted within the sequence of sheared and partially extensionally deformed mafic to intermediate volcanic and less mafic intrusion as well as intermediate volcanic and intrusion rock formations associated with quartz-carbonate vein and veinlet system and the main alteration products of chloritization, biotitization and carbonatization, and less silicification.

Property summary

The property is prospective for both orogenic gold and polymetallic VMS-style (volcanogenic massive sulphide) mineralization and comprises 212 mineral claims totalling about 119.5 square kilometres, located within the prolific Val d'Or mining camp between Probe Gold's McKenzie Break deposit (25.5 million tonnes grading 1.77 grams per tonne gold, 1,452,261 ounces inferred) to the north and Probe's Novador development project to the south (177.5 million tonnes grading 1.12 g/t Au, 6,405,000 ounces measured and indicated, and 30.3 million tonnes grading 1.59 g/t Au, 1,550,200 ounces inferred).

Note: Readers are cautioned that the geology of nearby properties is not necessarily indicative of the geology of the company's properties.

The company's multiphase drill program includes 75 drill holes that have been designed based on all the available historic and recently conducted information layers, including geological mapping and surveying, airborne geophysics, ground geophysics, geochemical surveys, and historic and recent drill program results.

The multiphase drill program includes five promising target areas: Gustav Cere, Val Saint George, Contact, Vert Lake, Golden Island Fault and Milieu Lake Batholite.

Historic drilling in the 1980s (AHS series, GM41852) targeted a horizon of gold-bearing quartz veins along the footwall of the Senneville komatiite. Recent drilling, in 2012 (SV-12-03, GM68366) and 2021 (XR-21-01A, GM72154), intersected higher gold-grade drill intercepts (up to 18.75 g/t Au over 0.85 metre) along the hangingwall contact of the Senneville komatiite, where relatively minor drilling has been focused. A third horizon of gold mineralization is suggested by the presence of visible gold in 1981 drill hole SNF-3 ("a few small pinpricks of visible gold," GM37553); however, assays are not reported for this interval.

Qualified person

Babak V. Azar, PGeo, Geo (EGBC No. 62313, OGQ No. 10876), an independent qualified person as defined by the National Instrument 43-101, has reviewed and approved the technical contents of this news release.

About Troubadour Resources Inc.

Troubadour Resources is a North American mineral acquisition and exploration company focused on the development of quality critical mineral and precious metal properties that are drill ready with high upside and expansion potential. Based in Vancouver, B.C., Troubadour trades on the TSX Venture Exchange under the symbol TR, on the OTC Markets under the symbol TROUF, and on the Frankfurt, Berlin and Tradegate stock exchanges under the symbol 2QD0/WKN:A3DBDE.

We seek Safe Harbor.