Troubadour Resources Inc. announce the results of its recently completed Induced Polarization (IP) Survey at the Senneville Copper-Gold property ("Senneville" or the "Property") in the eastern Val d'Or district. The Property is prospective for both orogenic gold and polymetallic VMS-style mineralization and comprises 255 mineral claims located in the eastern part of the Abitibi Greenstone Belt, approximately 25 km northeast of the gold mining center of Val-d'Or, Quebec. It covers over 12,000 ha of ground and is contiguous with Probe Gold's Val d'Or East properties to the north and south, which host a combined resource of 6.7 Moz gold measured and indicated and 3.3 Moz gold inferred.

The survey identified chargeability anomalies along the hanging wall and footwall contacts of the Senneville Komatiite in areas where there had been no previous diamond drilling. These zones are within areas host to previously proposed diamond drillholes, where work by the previous claimholder had returned Ag, Cu, and Zn metal anomalies. The Company has adjusted the location of the previously proposed diamond drillholes to ensure the chargeable zones are tested in the upcoming maiden drill program.

Val d'Or based geophysical contractor Geophysique TMC conducted the IP survey, which was focussed on the vicinity of the historic Gustave-Cere gold showing. The results from the survey highlight chargeability anomalies along the hanging wall and footwall contacts of the Senneville Komatiite, reinforcing Troubadour's exploration hypothesis that zones of mineralization are localized along the contacts of this geologic marker unit. Troubadour had proposed diamond drill holes along the untested strike length of the komatiite contacts as historic work was not focused here, and has now modified the previously proposed drillholes to intersect this chargeable zone.

The two principal target zones are described below. Target Zone 1: Southeast of the Gustav Cere gold showing, a continuous zone of elevated chargeability coincides with the southern contact of the Senneville Komatiite. Despite being on trend with the historic gold showing and along the same geologic horizon, this trend has never been tested with diamond drilling.

A MMI survey by the previous claimholder, Xander Resources, generated overlapping Ag, Cu, and Zn anomalies within this area that overlie the chargeable zone identified here. Target Zone 2: Approximately 800 metres northwest of the Gustav Cere gold showing, a discrete chargeability high aligns with the northern contact of the Senneville Komatiite, the same unit associated with gold mineralization at the Gustav Cere gold showing. Northwest of this chargeability anomaly, the previous claim holder Xander Resources, intersected a 10 meter wide blue-grey quartz vein that returned a widespread Ag anomaly (10.7 g/t Ag over 12.23m an up to 250 g/t Ag over 0.3m) along the same geologic contact, suggesting the mineralized veins extend to the northwest.

At the Gustave Cere gold showing, high-grade gold (up to 18.75 g/t Au over 0.85 meters, based on historical results) is hosted in quartz-carbonate-tourmaline veins that bear many similarities to the gold-bearing veins of the neighbouring Novador deposits. This showing has been defined by drilling for approximately 361 meters along strike, but step outs along the strike length of the controlling geologic structure have been limited. Sulphide mineralization at the Gustav Cere showing consists of haloes of disseminated to stringer pyrite that mantle the gold-bearing veins.