HALIFAX, NS,
June 28,
2022 /CNW/ - Fortune Bay Corp. (TSXV: FOR) (FWB: 5QN)
(OTCQX: FTBYF) ("Fortune Bay" or the "Company") is pleased to
announce initial drill results for its 100% owned Strike Uranium
Project ("Strike" or the "Project"), located in northern
Saskatchewan (see Figures 1 and
2). A total of nine drill holes were completed comprising 2,064
metres. Results included shallow intersections of elevated
radioactivity, between 35 and 95 metres below surface, within
favorable geological settings for high-grade, basement hosted
deposits typical of the Athabasca
Basin.
Highlights:
- Elevated radioactivity of over 300 counts per second ("cps")
was intersected in four of the nine drill holes completed (Table
2). The elevated radioactivity was associated with prospective
graphitic faults and favorable hydrothermal alteration:
-
- Drill hole S22-013 (K3 target) intersected an average of 840
cps from 145.5 to 145.8 metres (approximately 90 metres below
surface), including 1,800 cps from 145.7 to 145.8
metres.
- Drill hole S22-005 (Tena target) intersected an average of 365
cps from 82.1 to 84.1 metres (approximately 70 metres below
surface), including 1,300 cps from 82.3 to 82.4 metres.
- Drill hole S22-006 (Tena target) intersected an average of 390
cps from 106.9 to 107.5 metres (approximately 95 metres below
surface), including 500 cps from 107.0 to 107.1 metres.
- Drill hole S22-010 (K4 target) intersected 300 cps from 53.8 to
53.9 metres and 330 cps from 55.0 to 55.1 metres (both
approximately 35 metres below surface). These shallow intersections
conform with a new discovery of radioactive showings on surface
with radioactivity of up to 5,000 cps. An average of 340 cps
was also intersected from 135.1 to 135.4 metres (approximately 80
metres below surface).
- Drill hole S22-013 and S22-010 are located approximately 1.1
kilometres apart along the same graphitic unit (K-conductor),
defining a trend for follow-up. Nearby historical surface grab
samples include HY080 1.51% U3O8, Stancliff
0.19% U3O8, and Hacker Atompower 0.13%
U3O8 (see Figure 3).
Dale Verran, CEO for Fortune Bay,
commented, "We are very pleased with the initial results from
the maiden exploration drilling program at the Strike Uranium
Project. This was the first drill program aimed at testing the
extensive electromagnetic conductors on the project at shallow
depths, and the results have identified the key ingredients for
high-grade, basement-hosted discoveries related to the Athabasca Basin. The intersection of elevated
radioactivity and favorable alteration, associated with prospective
graphitic structures, indicates the presence of a uranium
mineralizing system adjacent to the present-day edge of the
Athabasca Basin. Our experienced
technical team is particularly encouraged by the results from drill
hole S22-013 which was highlighted by 1,800 cps within a graphitic
fault with hydrothermal alteration, representing a priority area
for follow-up along the K-conductor. Laboratory uranium assay and
geochemical results, combined with structural analysis of drill
core and detailed surface mapping, will be utilized to plan a
follow-up program."
Mr. Verran further added, "Exploration drilling has now
commenced at the Murmac Uranium Project where the Company plans to
test a compelling set of eight to ten targets identified from
electromagnetic and gravity surveying in proximity to numerous
radioactive and uranium surface showings and/or favorable
structural features. We are looking forward to the continued
drilling results from our Strike and Murmac Uranium
Projects."
Strike Drill Results
Drill Program Summary
A total of nine drill holes
(2,064 metres) were completed during the period May 21 to June 15, 2022. Holes were drilled to
test the targets documented in the News Release dated April 26, 2022, which were refined following
completion of ground gravity surveying in May. Two holes were
drilled at the Tena target, a historical prospect where over 1,000
tonnes of uranium ore were mined in the 1950's with reported grades
of 0.6% to 3.5% U3O8. A third hole was
drilled at the Tena South target, a coincident gravity low and
electromagnetic ("EM") conductor immediately south of the Tena
prospect. The remaining six holes targeted discrete gravity lows
located along prominent EM conductor corridors (named "J", "K" and
"L") proximal to favourable geochemistry results and structural
features. Drill hole collar information is summarized in
Table 1 and drill hole locations are shown in Figure 3.
Table 1: Strike Drill Hole Summary.
Hole
ID
|
Target
|
Easting
|
Northing
|
Dip
|
Azimuth
|
Length
(m)
|
S22-005
|
Tena
|
609135.1
|
6601530.4
|
-50°
|
342°
|
152.0
|
S22-006
|
Tena
|
609080.7
|
6601509.9
|
-50°
|
342°
|
131.0
|
S22-007
|
Tena South
|
608954.6
|
6601392.9
|
-45°
|
155°
|
251.0
|
S22-008
|
L1
|
610086.2
|
6601679.4
|
-45°
|
315°
|
173.0
|
S22-009
|
J3
|
608637.9
|
6605013.5
|
-45°
|
225°
|
350.0
|
S22-010
|
K4
|
610188.5
|
6603465.7
|
-45°
|
100°
|
284.0
|
S22-011
|
L4
|
611726.0
|
6605012.0
|
-45°
|
300°
|
233.0
|
S22-012
|
J2
|
607786.3
|
6604938.2
|
-45°
|
145°
|
230.0
|
S22-013
|
K3
|
609312.7
|
6602761.6
|
-45°
|
115°
|
260.0
|
Notes: Coordinates are
reported in UTM NAD83 Zone 12N. Azimuth is true north.
|
Initial Drill Results
The initial drill results for
each drill hole are summarized below, with final drill results to
be announced following receipt of uranium assay, geochemical and
reflectance data. Radioactivity results are presented as minimum
and maximum counts per second ("cps") recorded within the interval
reported, as measured by a Super-SPEC RS-125 handheld gamma-ray
spectrometer. A summary of any elevated radioactivity
(> 300 cps) encountered is provided in Table 2.
- Drill hole S22-005 (Tena) intersected a mylonitized
sequence of semipelitic to pelitic migmatite, diatexite and
granite. The Tena fault, a graphitic, brittle fracture zone with
hematization and chloritization, was intersected from 82.1 to 85.6
metres. Disseminated to fracture-hosted radioactivity averaging 365
cps (between 250 and 1,300 cps) is intersected from 82.1 to 84.1
metres (see Figure 4).
- Drill hole S22-006 (Tena) intersected a mylonitized
sequence of semipelitic to pelitic migmatite and diatexite. The
Tena fault, as described above, was intersected from 106.7 to 107.7
metres. Disseminated to fracture-controlled radioactivity averaging
390 cps (between 320 and 500 cps) was intersected in the fault from
106.9 to 107.5 metres. Drill hole S22-006 was a 60 metre step-out
west of S22-005.
- Drill hole S22-007 (Tena South) intersected a
mylonitized sequence of semipelitic to pelitic migmatite and
diatexite with intermittent quartzite units with locally elevated
sulphide content explaining the conductor target. No radioactivity
above background was observed.
- Drill hole S22-008 (L1) intersected a mylonitic sequence
of semipelitic gneiss, granite, and pelitic migmatite. Weakly
bleached and clay-altered rock was intersected (88.7 to 91.5
metres) associated with a brittle fault fracture zone (89.3 to 90.0
metres). Sheared graphite- and pyrite-bearing pelitic gneiss was
intersected from 125.5 to 136.3 metres with brittle fault
reactivation from 134.9 to 135.3 metres. Weak bleaching and
clay-coated fractures are associated with the fault zone. No
radioactivity above background was observed.
- Drill hole S22-009 (J3) intersected a mylonitized
sequence of semipelitic to pelitic migmatite and diatexite with
intermittent graphite-bearing pelitic gneiss (104.8 to 197.5
metres). The graphitic units are variably sheared with abundant
sulphide and brittle reactivation features. Weak bleaching occurs
sporadically in the graphitic shear zones. No radioactivity above
background was observed.
- Drill hole S22-010 (K4) intersected a mylonitic sequence
of semipelitic to pelitic migmatite and diatexite. Weak bleaching
and clay alteration, as well as weakly elevated radioactivity (up
to 330 cps from 55.0 to 55.1 metres), occurs locally in a sheared
and faulted section from 53.0 to 56.2 metres (see Figure 4).
Variably graphitic and pyritic pelitic gneiss occurs between 135.9
to 180.5 metres with abundant shearing and semi-brittle
deformation. Local sub-metre scale brittle fault reactivations
occur between 138.9 to 149.9 m, from
155.5 to 158.2 metres and 171.9 to 172.4 metres. Weakly elevated
radioactivity averaging 340 cps (between 300 and 400 cps) occurs
along foliation above the graphitic stratigraphy from 135.1 to
135.4 metres (see Figure 4).
The shallower intersection (53.0 to 56.2 metres) conforms with new
(not previously documented) radioactive showings discovered at
surface while collaring the drill hole. These showings are
associated with graphitic fault breccias in granitoid hosts with
radioactivity of up to 5,000 cps (see Figure 4).
- Drill hole S22-011 (L4) intersected a mylonitic sequence
of psammitic, semipelitic, and pelitic gneiss stratigraphy with
interleaved granite and graphite-bearing pelitic gneiss. The
dominant graphitic unit was intersected from 127.9 to 149.6 metres.
Weak to moderate bleaching occurs from 127.9 to 162.3 metres
associated with intermittent metre-scale graphitic faults. Local
high sulphide content is associated with sporadic quartz veining.
No radioactivity above background was observed.
- Drill hole S22-012 (J2) intersected a mylonitic sequence
of semipelitic to pelitic migmatite and diatexite, with variably
graphite-bearing pelitic gneiss from 79.6 to 153.1 metres with
intermittent graphitic shearing and brittle reactivation. Weak
bleaching and clay alteration occurs from 100.5 to 106.0 metres
associated with graphitic fault development. No radioactivity above
background was observed.
- Drill hole S22-013 (K3) intersected a mylonitic sequence
of semipelitic to pelitic migmatite to diatexite, with variably
graphite-bearing pelitic gneiss from 110.4 to 147.0 metres.
Graphitic shearing and semi-brittle deformation occur from 110.4 to
124.0 metres with a brittle overprint from 122.0 to 124.0 metres. A
zone of graphitic shearing and a reactivated graphitic fault with
hydrothermal alteration occurs from 143.3 to 147.0 metres and hosts
elevated radioactivity averaging 840 cps (between 300 and 1,800
cps) from 145.5 to 145.8 metres (see Figure 4).
Table 2: Summary of elevated radioactivity intersected.
Target
|
Hole
ID
|
Radioactivity
|
Association
|
Tena
|
S22-005
|
365 cps from 82.1 to
84.1 m, including 1,300 cps from 82.3 to 82.4 m
|
Graphitic brittle
fracture zone with hematization and chloritization – Tena
Fault.
|
Tena
|
S22-006
|
390 cps from 106.9 to
107.5 m, including 500 cps from 107.0 to 107.1 m
|
Graphitic brittle
fracture zone with hematization and chloritization – Tena
Fault.
|
K4
|
S22-010
|
300 cps from 53.8 to
53.9 m
330 cps from 55.0 to
55.1 m
340 cps from 135.1 to
135.4 m
|
Shallow radioactivity
hosted in graphitic faults.
Deeper radioactivity
associated with graphitic
pelite displaying shearing and brittle reactivation.
|
K3
|
S22-013
|
840 cps from 145.5 to
145.8 m, including 1,800 cps from 145.7 to 145.8 m
|
Reactivated graphitic
fault with disseminated to
vein-hosted occurrence associated with weak to moderate
hydrothermal alteration.
|
Notes: Radioactivity
measurement ("cps") is taken using a Super-SPEC RS-125 handheld
gamma-ray spectrometer. The cps values are averages for the
reported drill interval. The Company considers values > 300 cps
to be elevated for the Project.
|
Technical Disclosure
All drilling is being carried out
with NQ3 or NQ2 diameter. Radioactivity in counts per second
("cps") has been measured using a Super-SPEC RS-125 Spectrometer.
Individual measurements are taken over 0.1 metre core increments,
which is the approximate width of the instrument sensor, and
averaged over larger intervals where elevated. Core is removed from
the core box and moved, if necessary, to a location where the
instrument reads below background, and the measurement is collected
by placing the sensor against the core at the required location.
Background radioactivity is estimated at 200 cps, and values >
300 cps are considered to be elevated. The oriented drill cores are
being subjected to comprehensive logging and sampling to
characterize mineralization, alteration and structure. Samples will
be submitted to the Saskatchewan Research Council ("SRC")
Geoanalytical Laboratories (ISO/IEC 17025:2005 accredited) for
uranium assay and multi-element characterization.
Unless otherwise stated, the historical results (including drill
results) contained within this news release have not been verified
and there is a risk that any future confirmation work and
exploration may produce results that substantially differ from the
historical results. The Company considers these results relevant to
assess the mineralization and economic potential of the property.
Further details regarding the historical Tena prospect can be found
within the Saskatchewan Mineral Deposit Index (SMDA #1511). Further
details regarding the historical surface grab samples from HY080,
Stancliff and Hacker Atompower are available within Cameco Corp.
assessment reports filed on the Saskatchewan Mineral Assessment
Database (SMAD File Number 74N-0102, 74N-0103 and 74N-0106).
Qualified Person and Data Quality
The technical and
scientific information in this news release has been reviewed and
approved by Dale Verran, M.Sc.,
P.Geo., Chief Executive Officer of the Company, who is a Qualified
Person as defined by NI 43-101. Mr. Verran is an employee of
Fortune Bay and is not independent of the Company under NI
43-101.
About Fortune Bay
Fortune Bay Corp. (TSXV:FOR, FWB: 5QN, OTCQX: FTBYF) is an
exploration and development company with 100% ownership in two
advanced gold exploration projects in Canada, Saskatchewan (Goldfields Project) and
Mexico, Chiapas (Ixhuatán Project), both with
exploration and development potential. The Company is also
advancing the 100% owned Strike and Murmac uranium exploration
projects, located near the Goldfields Project, which have
high-grade potential typical of the Athabasca Basin. The Company has a goal of
building a mid-tier exploration and development Company through the
advancement of its existing projects and the strategic acquisition
of new projects to create a pipeline of growth opportunities. The
Company's corporate strategy is driven by a Board and Management
team with a proven track record of discovery, project development
and value creation. Further information on Fortune Bay and its
assets can be found on the Company's website at
www.fortunebaycorp.com or by contacting us as
info@fortunebaycorp.com or by telephone at
902-334-1919.
On behalf of Fortune Bay Corp.
"Dale Verran"
Chief Executive Officer
902-334-1919
Cautionary Statement Regarding Forward-Looking
Information
Information set forth in this news
release contains forward-looking statements that are based on
assumptions as of the date of this news release. These statements
reflect management's current estimates, beliefs, intentions, and
expectations. They are not guarantees of future performance. Words
such as "expects", "aims", "anticipates", "targets", "goals",
"projects", "intends", "plans", "believes", "seeks", "estimates",
"continues", "may", variations of such words, and similar
expressions and references to future periods, are intended to
identify such forward-looking statements. Fortune Bay Corp.
("Fortune Bay" or the "Company") cautions that all forward-looking
statements are inherently uncertain, and that actual performance
may be affected by a number of material factors, many of which are
beyond Fortune Bay's control. Such factors include, among other
things: risks and uncertainties relating to metal prices, changes
in planned work resulting from weather, COVID-19 restrictions,
availability of contractors, logistical, technical or other
factors, the possibility that results of work will not fulfill
expectations and realize the perceived potential of Fortune Bay's
mineral properties, uncertainties involved in the interpretation of
drilling results and other tests, the possibility that required
permits may not be obtained in a timely manner or at all, risk of
accidents, equipment breakdowns or other unanticipated difficulties
or interruptions, the possibility of cost overruns or unanticipated
expenses in work programs, the risk of environmental contamination
or damage resulting from the exploration operations, the need to
comply with environmental and governmental regulations and the lack
of availability of necessary capital, which may not be available to
Fortune Bay, acceptable to it or at all. Fortune Bay is subject to
the specific risks inherent in the mining business as well as
general economic and business conditions. Accordingly, actual, and
future events, conditions and results may differ materially from
the estimates, beliefs, intentions, and expectations expressed or
implied in the forward-looking information. Except as required
under applicable securities legislation, Fortune Bay undertakes no
obligation to publicly update or revise forward-looking
information. Fortune Bay does not intend, and does not assume any
obligation, to update these forward-looking statements, except as
required under applicable securities legislation. For more
information on Fortune Bay, readers should refer to Fortune Bay's
website at www.fortunebaycorp.com.
Neither TSX Venture Exchange nor its Regulation Services
Provider (as that term is defined in policies of TSX Venture
Exchange) accepts responsibility for the adequacy or accuracy of
this release.
SOURCE Fortune Bay Corp.