Barksdale Presents Positive Initial Geochemical and Geophysical Results at Sunnyside
BRO:TSXV BRKCF:OTCQB
BARKSDALE PRESENTS POSITIVE INITIAL GEOCHEMICAL
AND GEOPHYSICAL RESULTS AT SUNNYSIDE
January 30, 2019 – Vancouver, B.C. – Barksdale Capital Corp. (“Barksdale” or
the “Company”) (TSXV: BRO)(OTCQB: BRKCF) is pleased to report initial results from
its ongoing exploration programs (the “Program”) at its Sunnyside property, located
in southern Arizona, adjacent to South32’s Taylor-Hermosa development project.
To date, the Program has focused on the northeast quarter of the 5,223-acre
Sunnyside project, where the known extension of the Taylor- Hermosa zinc-lead-
silver-copper deposit continues onto Barksdale ground. This is a priority zone for
Barksdale as it sits within the footprint of the Company’s proposed drilling plans that
have been submitted to the US Forest Service for permit approval.
Surface Campaign
Barksdale’s team completed detailed mapping (1:6,000 scale) and extensive rock
chip sampling ( 1,904 samples) in the northern portion of the Sunnyside property
during 2018. T he surface campaign has identified multiple prominent mineralized
structural zones around the periphery of the Sunnyside porphyry complex, which was
partially defined by various ASARCO drilling campaigns in the 1960’s through 1980’s.
Individual assays from the Barksdale Program returned select high-grade results of
up to, and including, 15.75% copper, 19.15 g/t gold, 440 g/t silver, 6.54% lead, and
0.73% zinc, respectively. Comprehensive geochemical plots of copper, gold, silver,
lead and zinc can be found at the end of this press release (Figures 1 through 5).
Geochemical data is currently being analyzed and further evaluated using
geostatistical modeling software, such that project scale metal zoning patterns can
be established at Sunnyside. These models will be updated as additional surface
sampling is completed in 2019, which will likely see the sampling campaign extended
over the remainder of the Sunnyside property. Barksdale believes that these
mineralized structures likely represent leakage from larger mineralized bodies at
depth and will use these data to generate drill targets once the ongoing program are
completed.
Geophysical Surveys
Additionally, the Company initiated an initial 7-10 line-kilometer natural source audio
magneto-telluric survey (“NSAMT”) in October 2018, the purpose of which was to
gain subsurface structural data as well as to potentially identify Paleozoic carbonate
rocks (host rocks for the Taylor-Hermosa deposit) beneath volcanic cover. Based on
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the quality and depth of the data collected, Barksdale subsequently extended the
survey and ultimately completed 23.3 line -kilometers of NSAMT (Figure 6). Initial
results have identified numerous structural zones and geologic contacts at depths up
to, and in some cases, exceeding 2,500 meters depth (Figure 7) . A series of
prominent resistivity and conductivity anomalies have been identified to date and
Barksdale has engaged a third-party geophysical expert with extensive experience in
similar geologic systems to review and interpret the survey results. Barksdale will
provide additional updates to the market as these interpretations are finalized.
Target Generation
The Sunnyside-Taylor-Hermosa system is a very large mineralized system that has
yet to be fully explored. In particular, Barksdale’s ground has only seen a handful of
historic drill holes that targeted the skarn/ manto portion of the system that flanks
the Sunnyside porphyry to the east. All data indicates that the causative source of the
polymetallic copper-zinc-lead-silver replacement deposits at Taylor- Hermosa is the
Sunnyside porphyry c omplex located within Barksdale’s Sunnyside property.
Barksdale is focused on not only defining the size and quality of the mineralized zone
between the Sunnyside porphyry and the western edge of the Taylor-Hermosa
deposit ( the property boundary ), but also additional skarn/mantos around the
periphery of the Sunnyside porphyry.
Additional field and geophysical works for the 2019 field season are currently in
planning stage. The additional data collected during these programs will allow
Barksdale’s geologic team to build a portfolio of drilling targets that will be ranked,
prioritized, and then drilled once the requisite permits have been received.
Sampling and QA/QC
Surface samples reported herein are a combination of select, rock chip, float chip and
channel chip samples. Samples were taken under the direction of qualified geologists
and adhered to strict QA/QC programs. Samples were labeled, sealed and delivered
to ALS laboratories in Tucson, Arizona . All samples were dried, crushed and
pulverized with the pulps being analyzed by ALS in Vancouver, British Colombia,
Canada. Systematic assaying of standards, blanks, and duplicates is performed for
precision and accuracy. Analysis for 33 element four acid ICP AES with gold analysis
by fire assay with an AA finish.
Lewis Teal, Barksdale’s project manager and a “qualified person” as defined by NI
43-101, Standards of Disclosure for Mineral Projects is responsible for approving the
scientific and technical information regarding Sunnyside contained in this news
release.
Barksdale Capital Corp. is a base metal exploration company headquartered in
Vancouver, BC, that is focused on the acquisition and exploration of highly
prospective base metal projects in the United States. Barksdale’s portfolio of assets
is located within a world- class base metal district in southern Arizona and are
surrounded by some of the world’s largest mining companies.
BRO:TSXV BRKCF:OTCQB
ON BEHALF OF BARKSDALE CAPITAL CORP
“Rick Trotman”
Rick Trotman
President and Chief Executive Officer
For more information please phone 778-558-7145, email
[email protected] or visit www.BarksdaleCapital.com.
Neither the TSX Venture Exchange nor its Regulation Services Provider (as that term is
defined in the policies of the TSX Venture Exchange) accepts responsibility for the adequacy
or accuracy of this news release.
CAUTIONARY STATEMENT REGARDING FORWARD -LOOKING INFORMATION: This
news release contains “forward-looking information” under applicable Canadian
securities legislation which relates to future events or future performance (including,
but not limited to, the Company’s future exploration plans for the Sunnyside
property) and reflects management’s current expectations and assumptions based
on information currently available to the Company. Readers are cautioned that such
forward-looking information is neither a promise nor guarantee, and is subject to
risks and uncertainties that may cause future results to differ materially from those
expected including, but not limited to, actual results of exploration activities,
environmental risks, future metal prices, operating risks, accidents, labor issues,
delays in obtaining governmental approvals and permits, availability of financing and
other risks in the mining industry. There are no known resources or reserves on the
Sunnyside property and the proposed exploration programs are exploratory searches
for commercial bodies of ore. In addition, the close proximity of the Company’s
Sunnyside property to South32’s Taylor-Hermosa deposit is not necessarily indicative
of the mineralization within the Sunnyside property. All forward-looking information
in this news release is qualified by these cautionary statements and those in our
continuous disclosure filings available on SEDAR at www.sedar.com. Accordingly,
readers should not place undue reliance on forward- looking information. The
Company disclaims any intention or obligation to update or revise any forward-looking
information, whether as a result of new information, future events or otherwise, except
as required by law.
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Figure 1. Rock chip sample locations showing lead values in ppm . The surface projection of the currently defined
Taylor-Hermosa zinc-lead-silver-copper deposit footprint is highlighted in gray. The known deposit and mineralized
system remains open on the Sunnyside property to the NW and SW.
Figure 2. Rock chip sample locations showing copper values in ppm. The surface projection of the currently defined
Taylor-Hermosa zinc-lead-silver-copper deposit footprint is highlighted in gray. The known deposit and mineralized
system remains open on the Sunnyside property to the NW and SW.
BRO:TSXV BRKCF:OTCQB
Figure 3. Rock chip sample locations showing gold values in ppm. The surface projection of the currently defined
Taylor-Hermosa zinc-lead-silver-copper deposit footprint is highlighted in gray. The known deposit and mineralized
system remains open on the Sunnyside property to the NW and SW.
Figure 4. Rock chip sample locations showing silver values in ppm. The surface projection of the currently defined
Taylor-Hermosa zinc-lead-silver-copper deposit footprint is highlighted in gray. The known deposit and mineralized
system remains open on the Sunnyside property to the NW and SW.
BRO:TSXV BRKCF:OTCQB
Figure 5. Rock chip sample locations showing zinc values in ppm. The surface projection of the currently defined
Taylor-Hermosa zinc-lead-silver-copper deposit footprint is highlighted in gray. The known deposit and mineralized
system remains open on the Sunnyside property to the NW and SW.
BRO:TSXV BRKCF:OTCQB
Figure 6. Station locations for the NSAMT survey.
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Figure 7. NSAMT section line 200. The black dashed line is the interpreted contact between Paleozoic carbonate
rocks and overlying volcanic units.