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[Savannah-help-public] Money Makers


From: cklautky
Subject: [Savannah-help-public] Money Makers
Date: Sat, 21 Jan 2006 01:18:00 -0500

This One is Strong UP 0.06 (4.17%) Jan 20th Alone
Huge PR Campaign Running for Monday Jan 23th
We expect explosive growth on Monday
 
Infinex Ventures Inc. (IFNX)
 
Current Price: 1.50 UP 0.06 (4.17%)
 
OTC: IFNX.OB
 
Hot News Out
 
LAS VEGAS, Jan. 18 /PRNewswire-FirstCall/ - Infinex Ventures Inc. (IFNX:OB - News; "the Company") and its Board of Directors are pleased to announce that Infinex has increased its option in the Yew Claims to a 60% interest from the 55% interest originally agreed upon in the Joint Venture and Option Agreement dated June 14th 2004.
 
YEW CLAIMS
 
The Yew Claims are located on Texada Island, B.C. This region has a long history of mining dating back to 1876. Several high grade copper gold skarns were mined in the area. The geology of the Yew Claims is set out in MINFILE 092F/516 as follows:
 
"The area is dominated by Upper Triassic Karmutsen Formation (Vancouver Group) volcanic rocks consisting of typically fine-grained and/or feldspar phyric basalts and amygdaloidal basalts with minor intercalated limestone beds. At the Yew occurrence, stratigraphy is comprised of three rock units of the Karmutsen Formation. A lower, thick series of green-grey basalt flows that texturally change from amygdaloidal and non-amygdaloidal sequences, is overlain by a thin, white-grey fine-grained limestone that rapidly thins and thickens over short distances. Overlying the limestone is an amygdaloidal basalt breccia with fragments of amygdaloidal basalt up to 15 centimetres. White zeolites, epidote, pyrite, quartz and chlorite comprise vesicle fillings within the basalts. Two hundred metres north of the occurrence, two small diorite plugs intrude the basalts.
 
Massive pyrite, magnetite, pyrrhotite, minor chalcopyrite and trace bronite replaces limestone at the lower contact of the limestone bed. The mineralized zone is flat-lying, close to surface, thin and tabular, and ranges in thickness from 0.4 to 1.8 metres. Representative samples of the sulphide layer from a pit assayed up to 61.29 grams per tonne gold and up to 56.90 grams per tonne silver (Vancouver Stockwatch, January 19, 1988). A second zone comprising garnet-epidote skarn within basalt occurs below the massive mineralization and contains visible native gold. A drill hole intersection over 30 centimetres assayed 128.92 grams per tonne gold (Assessment Report 1486)."
 
DRILLING
 
In July of 2004 Infinex commenced its initial drill program on the Yew Property. The diamond drill program totalled 1,541.4 metres via 25 drill holes. Nine (9) of these drill holes contained variable thickness of skarn associated mineralization carrying appreciable gold and accessory silver and copper values. The near surface mineral zone continues to be the most prospective zone of potential exploitation on the property. Gold values of interest were returned from 5 drill holes. Attached is a table providing assay data related to mineral intervals within these drill holes.

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