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Virginia Gold Mines: Update on Coulon and Corvet Projects, James Bay.


QUEBEC CITY, Quebec -- Virginia Gold Mines Inc. (TSX TSX Toronto Stock Exchange (TSE before April, 2002)
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:VIA) ("Virginia") is pleased to provide an update on its Coulon and Corvet projects located in the Caniapiscau and LG-4 areas, James Bay James Bay, shallow southern arm of Hudson Bay, c.300 mi (480 km) long and 140 mi (230 km) wide, E central Canada, in Nunavut Territory between Ont. and Que. Numerous rivers flow into the bay; many of these have been developed for hydroelectric power in Quebec (see , Province of Quebec.

COULON

In the summer of 2004 Virginia and partner Noranda Inc. ("Noranda") completed an exploration program that consisted of eight (8) holes (CN-04-18 to 25) and surface work on the Coulon property. An agreement, signed in June 2004, granted Noranda the option to acquire a 50% interest in the Coulon property, in return for $8 million in exploration work and for a payment of $250,000 over the next seven years. The agreement also stipulates that Noranda must invest a minimum of $1 million per year and that Virginia will be the project's operator until a positive pre-feasibility study is completed, which study would then justify the completion of a feasibility study "A Feasibility Study" is an episode of the original The Outer Limits television show. It first aired on 13 April, 1964, during the first season. It was remade in 1997 as part of the revived The Outer Limits series with a minor title change. .

Work conducted in the DOM NORD Nord (nôr), department (1990 pop. 2,533,000), N France, bordering on the North Sea and Belgium. Lille is the capital.  area outlined a bimodal bi·mod·al  
adj.
1. Having or exhibiting two contrasting modes or forms: "American supermarket shopping shows bimodal behavior
 volcanic sequence more than 500 m thick, currently interpreted as a homoclinal sequence facing to the east. The sequence consists mainly of flows and felsic fel·sic  
adj.
Containing a group of light-colored silicate minerals that occur in igneous rocks.



[fel(dspar) + s(ilica) + -ic.
 tuffs, porphyric andesites, basalts and diverse sedimentary sed·i·men·ta·ry   also sed·i·men·tal
adj.
1. Of, containing, resembling, or derived from sediment.

2. Geology Of or relating to rocks formed by the deposition of sediment.
 assemblages. In the summer of 2004, two holes (CN04-22 and 23) tested the vertical extension of lens 08, which is located near the base of this sequence. Lens 08 was intersected in the winter of 2004 by hole CN04-08 (0.59% Zn, 1.31% Cu, 12.63 g/t Ag and 113 ppb ppb
abbr.
parts per billion
 Au over 38.13 m), hole CN04-15 (0.29% Zn, 1.29% Cu, 11.22 g/t Ag and 115 ppb Au over 12.27 m) and hole CN04-12 (5.8% Zn, 0.23% Pb, 0.28% Cu and 19.95 g/t Ag over 1.9 m) (see news release of April 29, 2004). On section 17N, hole CN04-22 has intersected 100 m vertically, under hole CN04-08, an intense alteration zone of 60 m thick but it did not show any significant mineralization Mineralization
The process by which the body uses minerals to build bone structure.

Mentioned in: Rickets

mineralization,
n the bioprecipitation of an inorganic substance.
. On section 18N, hole CN04-23 has intersected, to a vertical depth of 140 m (70 m under hole CN04-12), a zone of massive sulphides that graded 12.65% Zn, 1.54 % Pb, 1.36% Cu, 125.31 g/t Ag and 0.3 g/t Au over 4.7 m. Lens 08 is open at depth and towards the north. This same stratigraphic stra·tig·ra·phy  
n.
The study of rock strata, especially the distribution, deposition, and age of sedimentary rocks.



strat
 horizon also comprises, on section 13N, another volcanogenic vol·ca·no·gen·ic  
adj.
Of volcanic origin.
 sulphide sulphide: see sulfide.  zone discovered in the winter of 2004 in hole CN04-10 (2.83% Zn, 0.63% Cu and 20.34 g/t Ag over 3.07 m). This second zone was not tested in the summer of 2004 and remains open in all directions.

Hole CN04-25 on section 19N intersected a new volcanogenic sulphide zone named lens 09-25, which graded 2.91% Zn, 0.13% Pb, 1.12% Cu, 34.25 g/t Ag and 0.29 g/t Au over 21.8 m. Lens 09-25, located in the stratigraphic sequence approximately 200 m above lens 08, correlates with a significant alteration zone crosscut in the winter of 2004 by hole CN04-09. No other hole has tested this new fertile horizon and lens 09-25 is open at depth and towards the north. Hole CN04-25 replaced hole 24, which had to be abandoned for technical reasons.

Hole 25 also intersected another mineralized min·er·al·ize  
v. min·er·al·ized, min·er·al·iz·ing, min·er·al·iz·es

v.tr.
1. To convert to a mineral substance; petrify.

2. To transform a metal into a mineral by oxidation.

3.
 zone that graded 2.28% Zn, 0.68% Pb, 0.14% Cu and 44.23 g/t Ag over 2.3 m. This zone represents a third favourable contact and is located between the horizons hosting lenses 08 and 09-25. Mineralized intersections obtained in the winter of 2004 in holes CN04-12 (0.52% Zn and 15.5 g/t Ag over 2.22 m) and CN04-13 (1.62% Zn and 10 g/t Ag over 1.03 m) are also located at this contact. To date three (3) stratigraphic horizons fertile in volcanogenic mineralization have been outlined within the volcanic sequence of the DOM NORD area.

A similar volcanic sequence was also defined in the DOM area. Lens 16-17, which graded 9.94% Zn, 2.12% Pb, 0.73% Cu and 96.38 g/t Ag over 19.5 m in hole CN04-17, is located nearby the base of the sequence and occupies a stratigraphic position similar to that of lens 08 of the DOM NORD area. Stripping conducted in the summer of 2004 has exposed at surface that massive sulphide lens, which has returned values of 4.87% Zn, 0.38% Pb, 1.01% Cu and 57.1 g/t Ag over 15.6 m in channel sampling. Holes CN-04-18 to 21 have tested the extension of lens 16-17 to a vertical depth of 75 m, between sections 3N and 5N. Hole 21 (section 3N)and hole 19 (section 4N) have intersected interesting alteration zones but no significant mineralization is developed. In hole 18 (section 4+50N), the favourable contact zone is host to a pegmatite pegmatite: see granite.
pegmatite

Almost any wholly crystalline igneous rock that is at least in part very coarse-grained, the major constituents of which include minerals typically found in ordinary igneous rocks (such as granites) and in which
 intrusion of approximately 20 m thick. Hole 20 (section 5N) intersected the favourable contact without finding alteration or mineralization. Despite the lack of mineralization at a depth of 75 m, this favourable contact is still very promising since Deep EM anomalies were detected at depth, towards the south. Moreover, another mineralized horizon is present in the DOM area. Located about 20 m above the contact hosting lens 16-17, this horizon returned some significant intersections including 1.22% Zn, 3.97 g/t Ag over 3.7 m (CN04-18) and 3.3% Zn, 0.18% Pb, 0.17% Cu and 29.66 g/t Ag over 1.8 m (CN04-20). This horizon, which previously yielded some interesting intersections in the winter of 2004, would be the stratigraphic equivalent of the zone having graded 2.28% Zn, 0.68% Pb, 0.14% Cu and 44.23 g/t Ag over 2.3 m in hole 25 of DOM NORD. Finally the stratigraphic contact holding lens 09-25 of DOM NORD has not yet been tested in the DOM area and represents an additional target.

Work conducted in the summer of 2004 has also permitted the tracing of the lateral extensions of the fertile volcanic sequence over a distance of more than 12 km. Some new mineralized showings with values anomalous in base metals have already been discovered by prospecting and many airborne EM conductors remain unexplained unexplained
Adjective

strange or unclear because the reason for it is not known

Adj. 1. unexplained - not explained; "accomplished by some unexplained process"
 within this favourable sequence.

Virginia and partner Noranda are very pleased with these results, and in the winter of 2005 the partners intend to initiate an intense exploration program that will consist of geophysics geophysics, study of the structure, composition, and dynamic changes of the earth, its atmosphere, hydrosphere and magnetosphere, based on the principles of physics.  and a 4000 to 5000 m drill program.

CORVET EST EST electroshock therapy.

EST
abbr.
electroshock therapy
 

In the summer and fall of 2004 Virginia also drilled 16 holes (CE04-22 to 37) totalling 3186 m on its Corvet Est property (100% Virginia). The parameters of this drill program are reported in the annexed table.

Eigth (8) additional holes (CE04-22 to 25, 31, 32, 33, and 36) have tested the Marco zone between levels -125 and -200 m. All holes have intersected the gold structure and many sub-economic to economic intersections were obtained. Best results were:2.10 g/t Au over 46.0 m, including 4.50 g/t Au over 10.0 m (CE04-23), 6.81 g/t Au (cut) over 4.8 m (CE04-22), 2.14 g/t Au over 25.3 m (CE04-32), 2.33 g/t Au over 11.7 m (CE04-31) as well as 1.59 g/t Au over 13.0 m including 5.91 g/t Au over 2.0 m (CE04-24). A longitudinal section of the Marco zone follows.

The Marco zone is associated with a magnetic anomaly Magnetic Anomaly may refer to:
  • Kursk Magnetic Anomaly
  • Tycho Magnetic Anomaly
 that is followed over more than 3 km laterally on the property. Three (3) new holes (CE-04-34, 35 and 37) have tested the lateral extension of this magnetic anomaly. Hole CE-04-34 has intersected an altered zone similar to the Marco zone, with several mineralized intervals, including 2.60 g/t Au over 5.0 m, 2.56 g/t Au over 3.0 m and 3.53 g/t Au over 4.0 m. This hole is located 700 m west of the Marco zone and tested the vertical extension of an intersection that had yielded 1.32 g/t Au over 7.75 m in hole CE-04-16 during the winter of 2004. Hole CE-04-35, located 400 m west of the Marco zone, has intersected a mineralized zone grading 4.99 g/t Au over 2.0 m. Hole CE-04-37, located 2 km east of Marco, has not intersected significant mineralization.

Furthermore, five (5) holes (CE04-26 to 30) were drilled in the Contact zone to test the extensions of the intersections obtained in the winter of 2004 in holes CE04-14 (10.29 g/t Au over 4.75 m) and CE04-11 (5.49 g/t Au over 6.0 m) (news release of May 4, 2004). On the whole, new holes have intersected thinner intervals with values varying from 1.01 to 11.81 g/t Au. Complete drill results are presented in the attached tables.

Work is carried out by under the supervision of Geological Engineer, Paul Archer. He is a qualified person (as defined by National Instrument 43-101) and has more than 20 years of experience in exploration.

In 2004 Virginia has set up an Analytical Quality Assurance Program to control and assure the analytical quality of assays in its gold exploration. This program includes the systematic addition of blank samples and certified See certification.  standards to every batch samples sent for analysis at commercial laboratories. Blank samples are used to check for possible contamination in laboratories while certified standards determine the analytical accuracy and precision.

Samples are sent for assaying to Laboratoire Expert Inc. in Rouyn-Noranda. Samples are assayed by fire-assay followed by atomic absorption or gravimetry gra·vim·e·ter  
n.
1. An instrument used to measure specific gravity.

2. An instrument used to measure variations in a gravitational field.
 according to according to
prep.
1. As stated or indicated by; on the authority of: according to historians.

2. In keeping with: according to instructions.

3.
 industry standards. Repeats are carried out on mineralized intersections of interest and on the majority of the samples containing 1 g/t Au or more.

Virginia Gold Mines Inc. is among the most active mining exploration companies in Quebec with a working capital of over $17 million, debt free, and with approximately 36 million shares issued and outstanding. Virginia's shares trade on the Toronto Stock Exchange Toronto Stock Exchange (TSE)

Canada's largest stock exchange, trading approximately 1,200 company stocks and 33 options.
 (TSX) under the symbol VIA. Virginia concentrates its activities on its numerous properties spread over the vast unexplored regions of northern Quebec.

Tables of drilling results are available on CCNMatthews' website at the following address:

http://www2.ccnmatthews.com/database/fax/2000/corveta.pdf

A map related to the Corvet Project is available on CCNMatthews' website at the following address:

http://www2.ccnmatthews.com/database/fax/2000/corvet.jpg

VIRGINIA GOLD MINES INC. (TSX:VIA)
COPYRIGHT 2004 Business Wire
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Copyright 2004, Gale Group. All rights reserved. Gale Group is a Thomson Corporation Company.

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Publication:Business Wire
Geographic Code:1CANA
Date:Nov 15, 2004
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