Troubadour Resources Inc. provided an update on the Company's maiden drill program at its 100% owned Amarillo Project located approximately 30 kilometres west of the town of Peachland, British Columbia. The magnitude of hydrothermal alteration, sulphide mineralization and structural features observed in the drilling thus far, exhibit defining characteristics of the nearby Brenda Deposit. The alteration patterns and mineralization align well with this type of propyllitic alteration dominant copper porphyry deposit and indicate the potential for a more prolific zone nearby. Assays for all drill holes are pending. Drill holes AMAR18-01, AMAR18-02 and AMAR18-04 targeted the near surface moderate and shallow NE-SW trending Trench Chargeability Anomaly. All three drill holes intersected an altered and deformed granodiorite hosting narrow intervals of overlapping potassium, chlorite, silica, sericite, and localized epidote alteration frequently associated with vein-hosted and finely disseminated pyrite with trace amounts of chalcopyrite mineralization. The chargeability response is explained by finely disseminated sulphides and possibly clay alteration. Drill holes AMAR18-01 and AMAR18-03 were designed to test the deeper, strong and broader component of the Trench Chargeability Anomaly. Of significant interest, was the presence of altered porphyry dikes below 250 metres drill depth in drill hole AMAR18-01, displaying varying degrees of sericite and hematite alteration associated with finely disseminated grains of magnetite and pyrite.