Financial Statements |
TRS.CDNX Consolidated Financial Statements |
QUARTERLY REPORT -
AUGUST 31, 2001 |
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MANAGEMENT DISCUSSION
Nature
of Business: The
Company is an active junior mineral resource exploration company focused
on the acquisition, exploration and development of precious metals, base
metals and diamond projects. Properties
which the Company currently owns or which it is currently evaluating for
acquisition are located in the traditional mining areas of Ontario,
Canada. The
recoverability of the amounts comprising mineral properties and deferred
exploration costs is dependent upon the confirmation of economically
recoverable reserves, the ability of the Company to obtain the necessary
financing to successfully complete its exploration and development and
upon future profitable production and royalties. Risks: The
success of the Company’s business is subject to a number of factors
including but not limited to those risks normally encountered in the
mining industry such as exploration uncertainty, lack of operating cash
flow, increasing environmental regulation, continued industry and public
acceptance, regulatory compliance, potential liability claims, general
markets and economic conditions, competition with Companies having greater
resources, and further capital requirements and the uncertainty of
obtaining required financing. A
998 metre diamond drill program, in six holes, was carried out on the Mann
property, comprising 19 contiguous claim units (304 hectares) covering part of a
large mafic/ultramafic complex located
approximately 47 kilometres northeast of Timmins, Ontario. The property is
situated within the Mann complex, a mafic/ultramafic layered intrusion which
hosts Platinum Group Elements (PGE) and copper-nickel sulphide mineralization.
Broadlands Resources Ltd. is earning up to 50% interest in the property
as per an Agreement executed on November 9, 2000.
Phase I exploration included geological studies and the
re-logging and sampling of approximately 1,155 metres of historic drill core.
One hundred-four (104) samples were taken. Thirty-one (31) samples were
taken in clinopyroxenite of which twenty-four (24) are anomalous in PGE’s, up
to 942 ppb PGE’s plus gold. Phase
I geophysical surveys include 21 kilometres of Total Field Magnetics and 7.5
kilometres of Induced Polarization (IP) surveys. Whole rock analyses, thin section
and microprobe studies indicate that platinum group metals (PGM) and native gold
occur in discrete grains, approximately one to five microns in size.
The PGM are typically anhedral, and occur in clusters of two to ten
grains and comprise a complex suite of Pt, Pd, Te, Sb, Cu, Mn bearing minerals.
The PGM are generally enclosed in chlorite close to contacts with
secondary clinopyroxene or within secondary clinopyroxene and occur in proximity
to sulphides but rarely in contact with sulphides.
The sulphides consists of bornite, chalcopyrite, digenite and cobaltian
pentlandite. The
target of the most recent drill program was a clinopyroxenite horizon in the layered Mann ultramafic
complex which hosts highly anomalous platinum and palladium values. On the
claims, immediately north of the west end of the Frederick House River bridge,
three continuous chip samples taken by the Ontario Gological Survey returned
values of PGE + Au of 645 ppb over 12.20 metres, 574 ppb over 14.00 metres and 594
ppb over 22.00 metres. This unit
was intersected in three of six holes drilled.
It is a reasonably consistent unit ranging from 13 to 15 meter in true
thickness and dipping moderately to the east.
No anomalous PGM’s were returned from the clinopyroxenite where it was
intersected, but anomalous PGM values to 79 ppb were encountered in a coarse,
chaotic gabbro stratigraphically above the clinopyroxenite horizon.
In addition, six samples taken from drill hole M-01-3 returned highly
anomalous values in nickel. Six samples totaling 7.4 meters, were taken over a core
length of 92.5 meters and averaged 0.19% nickel.
Further work including geological mapping, detailed structural mapping,
sampling and diamond drilling is recommended. Temagami
Diamond Claim Project, Ontario, Canada On July 18, 2001, the Company acquired 100% undivided
interest in 837 mining claim units (the “Temagami Diamond Claims) in Hartle,
Askin, Burnaby, Eldridge, Flett, Gladman, Hebert and Kenny Townships, located
east of Marten River at the southern end of the Lake Timiskaming Structural Zone
near Sudbury, Ontario. The purchase
price for the claims is a cash
payment of $195,000 ($120,000 paid to September 30, 2001) and the issuance of
180,000 common shares of the Company (120,000 issued).
On September 20, 2001, the Company completed a Letter of
Intent executed in July 2001 to purchase 100% interest in
111 claim units in Hartle and Flett Township, adjoining the Company’s
existing 2,100 contiguous Temagami Diamond claims which cover approximately
34,000 hectares. The purchase price for the claims payable by the Company to
the Vendors is a cash payment of $25,000 (paid) and the issuance of 150,000
shares common shares of the Company (issued). The claims are considered
prospective for diamonds. The
Company’s Temagami Diamond Claim properties are located west of the
Timiskaming Structural Zone and straddle the Grenville Front, a deep rooted
structure that separates the thick Precambrian Superior craton from the
Grenville Province, a cratonized accreted mobile belt.
These deep-seated fault structures may have tapped into the diamond
bearing portions of the earth’s mantle.
The area exhibits many major north to northwest trending faults and
lineaments (associated with the Timiskaming Structural Zone) that intersect
major east to northeast trending structures.
The intersection of these deep-rooted structures may have provided an
excellent conduit or “plumbing system” for kimberlite or lamproite
emplacement. Dr.
Harrison Cookenboo, Ph.D., P.Geo. of Meridian Geoscience Ltd. was engaged in May 2001 to compile an independent evaluation report and to
provide recommendations for future exploration activities.
Dr. Cookenboo is interpreting proprietary data possessed by, or collected
by the Company in conjunction with recently released KIM data published by the Ontario Geological Survey (OGS).
To date, numerous kimberlite indicator minerals (KIM) have been
collected both on and immediately down-ice of the Company’s claims.
Included among these indicator minerals are sub-calcic G10 Cr-pyrope
garnets, eclogitic garnets and Cr- and Mg-rich chromites that are
compositionally similar to most such minerals included in diamonds.
Dr. Harrison Cookenboo believes that, “the Tres-Or property has the
potential to host significantly diamondiferous kimberlites due to its location
over Archean basement. The property
is near known kimberlites, in a direction of increasingly encouraging indicator
chemistry. The Tres-Or property
hosts indicator mineral suites suggestive of multiple kimberlite sources
including pipes that have sampled the diamond stability field in the mantle and
are likely to be diamondiferous.” During a recent site investigation, rock, till and beach
samples were collected to test selected high- priority target areas on the Tres-Or
property, as well as to establish rigorous protocols for subsequent regional
sampling programs. The
high-priority target areas were selected based on favourable indicator chemistry
and geological structures derived from both the OGS reports and Tres-Or’s
proprietary data. The favourable
indicator minerals include very sub-calcic G10 pyrope garnets comparable to the
best indicator minerals from producing diamondiferous kimberlites worldwide,
including the Ekati Mine in the
Northwest Territories. All of the
samples collected have been submitted for analyses, and the results will be
included in an independent evaluation report. The
Company is reviewing additional property opportunities and is actively pursuing
financing and discussing joint venture participation in the Temagami Diamond
Claim project with a number of interested parties. The Company has completed the Option Agreement to earn
its 100% interest in the Shallow River East and Northeast mineral claims
consisting of 52 units totaling 832 hectares.
The titles to the claims were transferred to the Company on July 27,
2001. Treasury shares will be
issued as the final property payment subject to filing with the Exchange an
acceptable geological report on the exploration work completed. The Company completed 300 metres of exploration
drilling on the Botany project to
test a 1.6 kilometre long geobotanical anomaly identified in earlier work
programs by John Mansville. Drilling
intersected massive to intermediate volcanics and gabbro and no significant base
metal mineralization was identified. Site
visits and prospecting and additional geochemical surveys were carried out
during the period. The Botany
Option Agreement is complete subject to the issuance of 100,000 shares of the
Company on approval of the Exchange of an acceptable geological report on the
exploration work completed. The
Company received confirmation of title transfer on October 5, 2001 of 26 mining
claim units covering 416 hectares in Warden Township. In addition, the Company staked 28 claim units contiguous and
adjoining the Botany claims. Earlier
exploration programs carried out by the Company on the Shallow River Project
identified a rhyolite porphyry unit which may be indicative of a
semi-conformable alteration zone related to a volcanogenic massive sulphide
(VMS) alteration system. The
prospective zinc-bearing felsic volcanic horizon has been identified over eight
kilometres of property length and remains open along strike.The properties are
located approximately 65 kilometres northwest of Kirkland Lake, Ontario, and
cover largely under-explored southeast trending package of felsic volcanic,
mafic volcanic and sedimentary rocks. In
August 2001, Mobile Metal Ion geochemical surveys were carried out over two
areas on the property to verify and better locate previously identified
anomalies. One hundred eighty-two
samples approximately 50 grams in weight were taken at 20 to 40 centimeters
depth, placed in zip-lock freezer bags and taken to Xral Laboratories in
Rouyn-Noranda for analysis using the MMI technique for Cu, Pb, Zn and Cd. Analyses of samples from the eastern grid were
less clear. No significant anomalies are apparent from this work. The
success of the sampling on the western grid indicate the MMI system works
in this terrain. There is a good possibility the eastern grid might not
have extended far enough to the north to cover the biogeochemical anomaly
outlined in 1972. The survey should be extended at least 200 metres
further north and all lines sampled.
Further work including mapping, prospecting and sampling is
recommended to evaluate the base metal potential of the Shallow River,
Shallow River East and Botany properties. The Company is pursuing joint
venture participation in the project. The Company has working capital of approximately $33,247 and
is pursuing a modest financing that will include a non-brokered private
placement of both equity and flow-through investments. Subsequent to the period, the Company received
Acknowledgement of Payment of $18,000 in full satisfaction of a judgment in the
Supreme Court of British Columbia on September 4, 1998 between R.A. Jones and
Associates Inc. and Sterling Pacific
Resources Inc. The Company has recovered expenses related to the acquisition
and exploration of the Mann Project by optioning 50% interest in the property to
Broadlands Resources Ltd. in a Letter Agreement approved by the Exchange
February 8, 2001. As at August 31,
2001, Broadlands has made cash payments to the Company totaling $13,000 and
issued 150,000 common shares. The Company continues with sampling and scientific
investigations on the Temagami Diamond Claims.
The most recent information and proprietary data is being presented to
several companies active or interested in acquiring diamond exploration
projects. The goal is to secure an
Option/Joint Venture agreement or obtain additional funding for continued
advancement of its properties. During the period, the Company completed a non-brokered
private placement of 723,500 units (323,500 being flow-through units) of the
Company at $0.25 per unit. Each
unit consists of one common share and one non-transferable share purchase
warrant. Each share purchase
warrant can be exercised to acquire one common share of the Company for a period
of one year at an exercise price of $0.50 per share.
Proceeds from the financing will be used for general working capital, and
for the acquisition and exploration of the Temagami Diamond Claims, located in
the Sudbury Mining Division of Ontario. During the period, the directors of the Company
exercised 394,576 stock options at $0.15 for net proceeds to the Company
of $59,186. The proceeds are to be
used for general working capital and for the acquisition and exploration of the
Temagami Diamond Claim project. Subsequently,
on July 23, 2001 the Company granted stock options to the directors and officers
of the Company to purchase an aggregate of 670,000 shares at an exercise price
of $0.14 per share for a three (3) year term. Warrants exercised during the period and up to the date of
this report include a total of 125,000 warrants exercised at $0.10 for net
proceeds of $12,500.
The
Company does not have any investor relations contracts.
Investor relations is managed by the Directors and includes daily contact
with shareholders and attendance at industry conferences and trade shows.
Other investor relations activities include maintaining the Company’s
web site, preparation and dissemination of documentation packages.
Liquidity and
solvency: The financial
statements presented in Schedule A, have been prepared on a going concern
basis which assumes that the Company will be able to realize its assets
and discharge its liabilities in the normal course of business for the
foreseeable future. The
continuing operations of the company are dependent upon its ability to
raise adequate financing, secure substantial option or joint venture
partnerships and to advance project opportunities to viable operations in
the future. |
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