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Yorbeau Reports Additional High Grade Mineralization at Scott Project
MONTRÉAL, QUÉBEC--(Marketwired - Jan. 6, 2016) - Yorbeau Resources Inc. (TSX:YRB.A) (the "Company" or "Yorbeau") is pleased to report on recent diamond drilling
About this update from Yorbeau Resources, Inc. Class A
[{"type":"text","content":" MONTRÉAL, QUÉBEC--(Marketwired - Jan. 6, 2016) - Yorbeau Resources Inc. (TSX:YRB.A) (the \"Company\" or \"Yorbeau\") is pleased to report on recent diamond drilling results at its 100% owned Scott Lake project in Quebec. Drill hole SC-82W intersected another higher grade massive sulphide zone approximately 45 metres updip from a similar intersection reported originally in hole SC-82 (October 29, 2015 press release). As was the case in SC-82, this shallower high grade massive sulphides intercept is located along the potential up-dip extension of the CFO Lens. Another mineralized interval was also obtained along the Gap Lens in hole SC-31W2. These mineralized intervals, as were all intercepts released by the Company since June, are located outside of the mineral resources as currently estimated (see attached Figure 1) at the Scott project. Assay results are shown below: DDH SC-82W Section 1900W (weighted averages) From (m) To (m) Length (m) Cu % Zn % Au g/t Ag g/t Remarks 588.6 593.6 5.0 0.7 12.1 0.2 10.2 massive sulphides (CFO horizon) including 588.6 589.3 0.7 3.6 22.2 0.6 26.3 massive and stringers sulphides DDH SC-31W2 Section 1900W (weighted averages) From (m) To (m) Length (m) Cu % Zn % Au g/t Ag g/t Remarks 853.0 884.0 31.0 1.0 1.4 0.2 28.2 stringers sulphides (Gap Lens) including 853.0 859.4 6.4 1.8 0.9 0.1 48.7 stringer sulphides and 876.0 884.0 8.0 1.0 1.7 0.2 32.3 stringer sulphides As this is still preliminary drilling on the above mineralization, the exact shape and true width cannot be determined with certainty. The core lengths obtained may not reflect the true width of the mineralization. The high grade massive sulphides (5.0 metres of 12.1% zinc and 0.7% copper) discovered at a depth of 588.6 metres are associated with a distinct mineralized horizon located about 100 metres to the north of the one hosting the newly discovered Gap Lens. These sulphides are associated with a rhyolite unit known as \"Tony Rhyolite\" and this interval is therefore interpreted as being located along the up-dip extension of the CFO Lens but at much shallower depth than indicated by previous work (see attached Figure 1). Hole SC-82W did not intersect mineralization along the Gap Lens. Indeed, at the targeted depth volcanic host rocks are cut by barren intrusive rocks associated with the Chibougamau Pluton. This situation is analogous to...