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GOLDEN
CHALICE RESOURCES INC.
711
– 675 West Hastings Street, Vancouver, B.C. V6B 1N2 (604)
685-2222 *Fax: (604) 685-3764
www.goldenchaliceresources.com
TSXV: GCR
FOR IMMEDIATE RELEASE�������������������������������������������������������������������������������������������������������������������
July 17, 2007����������������������������������������������������������������������������������������������������������������������������������������������
Golden
Chalice Resources Intersects Large Zinc Zone
on
the Abitibi East Property
Golden Chalice
Resources Inc. is pleased to announce the
discovery of a wide zinc mineralized zone in a geological setting similar to the world class Kidd Creek Deposit.�� The new zinc
discovery occurs on the
company’s Abitibi East Property located approximately 65 km east of
Xstrata’s zinc processing metallurgical facility in Timmins, Ontario.��
The Abitibi East Property is also located about 70 km north-east of the Company’s Langmuir Property where a new
nickel discovery was first announced on May 16, 2007.�� Drilling continues on both properties.�
Laboratory results for the Langmuir
Property drilling are expected to be received and announced later this week.
Drilling on the
Abitibi East Property in 1998 by previous operators first identified geology
favourable for hosting Volcanogenic Massive Sulphide (VMS) style zinc, lead,
copper mineralization similar to the
Kidd Creek Mine (117,547,000 tonnes @ 2.2% copper (Cu), 7.25% zinc (Zn), 0.28%
lead (Pb) and 147.43 g/t silver (Ag)).� The Kidd Creek deposit is associated
with felsic lava domes and cryptodomes that occur proximal to synvolcanic fault
zones.� The Company’s initial drilling in 2005 confirmed the VMS potential, intersecting 1.25% Zn, 0.13% Pb,
and 0.04% Cu over 4.5 metres of core length.� Systematic follow-up drilling
during 2006 and 2007 across what is considered to be a 6 kilometre wide basin
located the most favourable area for
more detailed drilling to discover a VMS deposit.
To date, a consistent horizon of
stringer and disseminated Zn, Cu and Pb mineralization with anomalous Ag has
been identified spanning a strike length of approximately 2.0 kilometers.��
Geological, geochemical (MMI), and geophysical (VTEM and IP) information have
been used to target and identify areas for testing mineralization at depth.
The new discovery was found with the first two holes drilled at depth on one of a
number of targets.� The results suggest that zinc mineralization is increasing
in tenor to depth. �The first hole was an extension of an earlier drilled hole,
Hole GCAE-07-02.� This hole, drilled at azimuth 195� and dip -50�, intersected
1.59% Zn, 0.41% Pb, and 0.02% Cu over 12.10 metres of core length from 391.5 to
403.6m.� The second hole GCAE-07-16, was drilled on the
same section with a collar 100 metres to the
north behind hole GCAE-07-02 and with a dip of -70�.� This deeper hole
intersected 2.00% Zn, 0.55% Pb, and 0.01% Cu over 10.0 metres of core length
from 668 to 678 metres, within a longer intercept of 1.61% Zn, 0.38% Pb, and
0.02% Cu over 20.9 metres of core length from 668 to 688.9 metres.� This larger
and more mineralized zone is more than 300 metres down dip of the zone in hole GCAE-07-02.
In addition, the
deeper hole not only intersected stringer and fracture filled zinc
mineralization, but also what appears to be replacement style mineralization.�
This is the first hole where zinc
rich bands appear to be replacing bedding.� This style of mineralization may be
an indicator of increased proximity to a massive sulphide zone.
Dr. George
Hudak, an Associate Professor at the
University of Wisconsin-Oshkosh and researcher on the
relationships between volcanology, hydrothermal
alteration and VMS deposits, has assisted Company geologists in the recognition of lithologies and alteration at the Abitibi East Property. �Dr. Hudak is currently
utilizing lithogeochemistry (rock chemistry) and petrographic studies
(microscope analysis of rock) to help vector (target) in on felsic domes and potential
synvolcanic fault zones which are often associated with VMS deposits.
The increase in size and strength of
the zinc mineralized zone at depth
combined with the recognition of
debris flows with felsic lava fragments and sulphidic clasts, graphitic and
cherty exhalites, moderate to strong silicification and sericitization,
stringer Zn, Cu and Pb mineralization, and replacement style mineralization in the drilling to date, support the
potential for a volcanogenic massive sulphide deposit on the
Abitibi East Property.�
A Summary of Volcanogenic Massive
Sulphide Deposit Environments and how they
relate to the Abitibi East exploration
is available on Golden Chalice Resources’ web site www.goldenchaliceresources.com
Further
drilling is planned to target the
downdip and strike extent of this newly discovered mineralization.� Peter Caldbick, P.Geo., is the
qualified person for the purposes of
National Instrument 43-101 and has read and approved this news release.
About Golden Chalice
Golden Chalice is
well positioned to discover and capitalize on world class gold, silver, copper,
nickel, zinc, platinum and palladium deposits.� During the
last couple of years the Company has
strategically accumulated large land packages in existing mining or mineral
districts such as the Abitibi in Ontario and the
Bathurst Camp in New Brunswick.�
These properties have existing infrastructure and are often within road access
to metallurgical facilities to process mined ores.� Details relating to
exploration activities on specific properties will be announced during the coming months as the
work program is implemented. �
GOLDEN CHALICE RESOURCES INC.
On behalf of the
Board of Directors
Richard
W. Hughes, Chairman
For Further
Information Contact: The Hughes Exploration Group
Phone: (604) 685-2222 or visit
Golden Chalice’s web-site: www.goldenchaliceresources.com
to see Smartstox interviews with Company Chairman and President.
This document
contains certain forward looking statements which involve known and unknown
risks, delays and uncertainties not under the
corporation’s control which may cause actual results, performance or
achievements of the corporation to
be materially different from the
results, performance or expectation implied by these
forward looking statements.
The TSX Venture
Exchange has not reviewed and does not accept responsibility for the adequacy or accuracy of this news release.