COQUITLAM, BC, Oct. 7 /CNW/ -- Supreme Resources Ltd. (Supreme) is pleased to provide an update on geophysical exploration results at its TAS (Copper) Project, located in the Copper Mountain Mining Camp, in the Similkameen Mining Division of southwest British Columbia.

Supreme has a large claim (1306 hectares) under option from Grant Crooker, P.Geo., situated immediately south and east of the property of Copper Mountain Mining Corp. (TSX.CUM) and staked claims to the south of the optioned ground. Additional claim staking has just been completed. The optioned claim has two Minfile showings (92H5 SE 192 and 193) explored in the past with geochemical and geophysical anomalies and known showings of copper mineralization. Other mineralized showings found by Grant Crooker in 1997 are not included in Minfile but are described in Assessment Report 25102 (Crooker, 1997).

An Interpretation Report by Quantech Geoscience Ltd. has recently been received describing a Titan 24 Deep Earth Imaging Survey completed earlier in the summer.

A Titan-24 survey was carried out over the TAS project area, British Columbia, Canada, between May 15th and June 1st 2009. The survey grid included five lines totaling 18 kilometers (19.5 km with extensions). The Titan 24 system is basically a deep Induced Polarization (IP) method used on the adjacent Copper Mountain porphyry copper-gold deposit.

Three lines were surveyed in the optioned claim and two lines in the claims to the south (Belgie Creek area) The data were inverted using 2D inversion algorithms to produce maps and sections showing resistivity and chargeability of the subsurface. The primary objective of the geophysical surveys was to locate potential copper mineralization targets to a depth of 750 m in the TAS claims area which could potentially be related to the mineralization found at the Copper Mountain mine, located adjacent to the TAS project.

Results

Results of the surveys are summarized from the Interpretation Report by A. Verweerd Dr. Rer Nat. (M.Sc. Equivalent) and Kevin Killin (Hon. B.Sc., of Quantec.

Northern area: The resistivity surveys on the northern lines show a conductive overburden of approximately 100 m thickness. However, The chargeability models of the northern group of lines show a large highly chargeable feature in the southern extent of all three lines, potentially outcropping on the west and dipping towards the north-east. A succession of north dipping fault-like features is also suggested, separating isolated chargeability features.

Southern Area: The two southern lines also show an extensive chargeability high in the southern portion of the lines, and the north dipping fault-like features. The northern portion of the lines only shows a very limited chargeability response.