Third Gold-in-Oxide Blanket Identified Within Cuiu Cuiu Gold District

VANCOUVER -  Cabral Gold Inc. reported on an initial 12 RC drill holes and three diamond holes drilled within and above the Central gold deposit within the Cuiu Cuiu gold district in northern Brazil. Highlights are: 1) DDH251, intersected gold-in-oxide mineralization at the Central deposit, and returned 55.1m @ 1.1 g/t gold from 4.9m depth, including 5m @ 6.1 g/t gold 15.5m @ 1.7 g/t gold from 65.8m depth, and 3.5m @ 0.8 g/t gold from 81.3m depth in un-weathered and highly brecciate and altered intrusive rocks beneath the oxidation. 2) DDH247, also drilled at Central, returned 11.0m @ 0.7 g/t gold from surface, in gold-in-oxide blanket material, as well as 20.4m @ 0.5 g/t gold and 23.3m @ 0.3 g/t gold in un-weathered and highly brecciate and altered intrusive rocks further down the hole. 3) Results on an initial 10 shallow RC holes drilled within and around the northern part of the Central deposit, revealed a thin but consistent gold-in-oxide blanket. Results of note include RC259 which returned 26m @ 0.4 g/t gold in oxidized material from surface.

Alan Carter, President and CEO, said, "The results from the initial drilling at the Central gold deposit clearly demonstrate that we have a significant zone of gold-in-oxide mineralization forming a blanket above the primary Central deposit. This is the third gold-in-oxide blanket identified at Cuiu Cuiu since the initial discovery at MG in April of last year, and these recent discoveries are in addition to the two existing hard-rock deposits with resources at Cuiu Cuiu. At this stage, we do not know the extent of the blanket or how much of this material at Central is in-situ weathered primary gold mineralization, and how much is transported cover material. Nevertheless, both types of material are expected to add significantly to the inventory of potentially leachable gold-in-oxide deposits recently identified at MG and PDM. Additional drilling over the next months is expected to further define the limits of the oxide material at Central, whilst providing further definition of the high-grade zones within the underlying primary deposit at Central."