due to doming of the greenstone sequence over the granitic intrusive. The most northeastern tip of the Kasubuya license encompasses some Upper Nyanzian Formation comprising well-exposed banded iron formation and felsic tuffs and poorly-exposed pillowed tholeiitic basalt lava and mafic tuffs typical of the Geita greenstone belt. Chibango Project The Chibango tenement is located within the central Lake Victorian goldfields region of Tanzania 10 km SW of the Geita town site and 6 km south of the Ridge 8 or Nyamulilima Hill gold deposit owned by AngloGold Ashanti. Access is via a sealed road that runs WSW from the town of Geita and crosses the extreme NW corner of the property at a distance of about 25 km. Topography is very hilly with thick native forests covering much of the property. The Chibango Project is hosted wholly within granite directly south of the regionally- and historically-significant gold-producing greenstone belt of the Geita goldfield south of Lake Victoria. Despite strong topography, actual outcropping granite is rare and largely obscured by the dense vegetation. Significant fracturing consistent with regional structures known to control the mineralisation at Geita and other prospects of the greenstone belt can be identified from the interpretation of regional aerial magnetic images. Northern Domain Nyasiri Project The Nyasiri tenement is located in northeast Tanzania within the historically productive Mara-Musoma Goldfield some 20 km SE of North Mara (Nyabirama) mine owned by Barrick Gold. The area is accessible by Tarime airstrip then a rough road going towards the Serengeti District; the tenement straddles the western border of the Serengeti National Park. The Nyasiri Project is hosted dominantly within granite that contains two small inliers of greenstone rocks (1 to 2 km and 2 to 3 km in area) presumably of Nyanzian origin. The western quarter of the property is covered with Bukoban Proterozoic-age sediments which unconformably overlie the Archean granite/greenstone beneath. Intrusive Proterozoic-age ultrabasic rocks occur along the southern margin of the property. Their sub-surface distribution is likely to be extensive as a gravity anomaly associated with the ultrabasic lopolith intrusion covers a large portion of the Nyasiri property. The Keserya Hills Cr-Ni-PGE prospect occurs immediately south of the Nyasiri property and the ultramafic rocks which host this prospect trend into the Nyasiri tenement. These ultramafic rocks are considered prospective for massive or disseminated Ni-Cu-PGE sulphide mineralisation or strataform Ni-Cr-PGE mineralisation. Buhemba South East Project The Buhemba South tenement is