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Please click on diagram and table for larger view in PDF BRAVOThe Bravo is a large mafic-ultramafic complex with many geophysical anomalies and nickel sulphide showings that spans over 4 km in length and 800 m wide. The Bravo complex is situated approximately 21 km northeast of the Getty zone, and was acquired from Novawest and Cascadia in 2007 (see press releases dated June 20, 2007 and August 17, 2007).
Geologically the immediate Bravo area has many extensive surface showings identified as B1 to B9, which are within a relatively large ultramafic-mafic complex. The Bravo-B9 showings are located in the eastern part of the Bravo complex. Grab sample assays of massive, semi-massive, net-textured and blebby sulphide bearing pyroxenite included results of up to 3.01% Ni, 0.89% Cu, 0.21% Co, 1.75 g/t Pt, and 2.34 g/t Pd (see press release dated September 14, 2007). 
The Bravo-B8 showing is located 200 m southwest of B9. Surface assays of massive and semi-massive sulphide bearing olivine pyroxenite included results of up to 1.80% Ni, 0.21% Cu, 0.13% Co, and 0.95 g/t PGE (see press release dated September 14, 2007). The Bravo-B6 showing is located 1 km southeast of B8. Surface assays of a sample of ultramafic containing gossan with disseminated sulphides included results of 0.56% Cu, 0.36 g/t Pt and 1.28 g/t Pd (see press release dated September 14, 2007).
Core library at the Belanger base camp The Bravo-B4 showings are located 1 km west of B6, in an area of a very strong airborne electromagnetic (VTEM) anomaly. Grab sample assays of pyroxenite with disseminated sulphides included results of up to 0.35% Ni, 0.56% Cu, and 1.35 g/t PGE (see press release dated September 14, 2007). The McCart Island showing is located 2 km southwest along strike of B4 on the Bravo claim block. The McCart ultramafics are part of the Bravo complex. Prospecting found frost heaved ultramafic rocks hosting weak disseminated and patchy nickel sulphide mineralization. Grab sample assays of a single sample included results of 0.58% Ni, 0.40% Cu, and 0.91 g/t PGE.
Goldbrook geologist John Bligh and President Brian Grant inspect latest drill core Forty-four drillholes have been completed on the Bravo complex for a total of 6,435.8 m, with the majority of drilling having occurred on the B4 prospect. Historic and previous drilling data indicates that Ni-Cu-PGE sulphide mineralization has been intersected intermittently for 300 m along strike and to depths up to 200 m below surface at Bravo B4. Higher grade intersections appear thicker but lower grade in the west, enclosed within larger lower grade halos, and underlain by copper and precious metal rich veins. The Bravo B4 prospect mineralization is shallow and remains open along strike and down-dip.
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