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Terra Rossa Gold Ltd. Provides Exploration, Development and Corporate Update Including Announces Extension of Warrants
VANCOUVER, British Columbia, April 01, 2026 (GLOBE NEWSWIRE) -- Terra Rossa Gold Ltd. (the Compan...
About this update from Terra Rossa Gold Ltd.
[{"type":"text","content":"Terra Rossa Gold Ltd. Provides Exploration, Development and Corporate Update Including Announces Extension of Warrants\nVANCOUVER, British Columbia, April 01, 2026 (GLOBE NEWSWIRE) -- Terra Rossa Gold Ltd. (the Company or TRG) (TSXV: TRR) is pleased to provide the following update on the exploration and development activities at the Company’s wholly owned Vetas Gold Project (Vetas) in the Santander gold district of Colombia. The Vetas Gold project is part of the Vetas-California gold district, a belt of epithermal gold occurrences of the intermediate -high sulfidation type. Gold-silver mineralization in the Vetas Gold project occurs in quartz veins and structures hosted in biotite gneisses representing the basement of the Precambrian Bucaramanga Complex, and in stockwork-type mineralization as a dense millimetric scale sets of veinlets adjacent to the high-grade quartz veins. At least three intrusive rock types have been recognized on the property intruding the gneiss, including a dacite porphyry. Recent work completed by the geology team has included reconnaissance geological mapping along the project area to identify the various lithologies and mineral associations – which has also identified several intrusive rock assemblages including a dacite porphyry. (See Photo 1). A review of the geophysical and geochemical data on rocks and soils has successfully integrated with the historical drillhole data within a 3D project model. (See attached map for location of ongoing geochemical and geophysical mapping), This will now be used as the basis for a detailed surface mapping campaign, followed up by a first pass surface drilling program scheduled to commence later in Q2/early Q3. The review of the data from the geophysical survey reveals anomalies in both chargeability and resistivity up to a depth of 200 m in the Real Minera zone and other prospective areas. The survey indicates a strong chargeability anomaly at 300 m deep towards El Dorado which is likely associated with the occurrence of granodiorite and tonalite which is also evidenced by surface outcrops and boulders. Anomalies partially coinciding with reported intrusive outcrops are pending to be tested in several other areas towards the NW and within San Bartolo mining title. Drilling will focus on these key areas and will be incorporated in the first stage dril...