VANCOUVER, BC, Dec. 7, 2020 /CNW/ - District Metals
Corp. (TSXV: DMX) (FRA: DFPP); ("District" or the
"Company") is pleased to report additional results from the
final airborne electromagnetic ("EM") and magnetic data that covers
the entire 5,144 hectare Tomtebo Property located in the Bergslagen
Mining District in south-central Sweden. A detailed heliborne
SkyTEM survey comprising approximately 600 line-km was flown at
100 m line spacing in July 2020, and geophysical interpretations were
successfully completed by Condor Consulting and Geovista AB.
Garrett Ainsworth, CEO of
District, commented: "We are very pleased with the SkyTEM results,
and the application of this modern exploration method has
undoubtably proven to be very successful. The recently flown survey
has identified numerous conductive and magnetic high anomalies that
showcases the exceptional potential to make additional polymetallic
discoveries across the Tomtebo Property.
Our last step before drilling anticipated in Q1 2021 will
include a targeted ground gravity survey over the Tomtebo Mine
Trend which will start shortly and help us refine and prioritize
existing targets within this important trend."
The SkyTEM results have been interpreted such that moderately to
strongly conductive zones represent targets for copper-gold
dominant sulphide mineralization, and non-conductive to weakly
conductive zones represent targets for silver-zinc-lead dominant
sulphide mineralization. Moderate to strong magnetic highs
represent targets for both types of sulphide mineralization.
No significant graphite-rich zones have been mapped or documented
on or around the Tomtebo Property, suggesting that any geologic
conductors are likely due to iron or polymetallic sulphide
mineralization.
SkyTEM Highlights – Tomtebo Property
- The previously reported 3 km long Tomtebo Mine
Trend (refer to October 15, 2020
news release) has been extended to 4.7 km long. This
trend comprises numerous magnetic high anomalies (A to C) and
conductive anomalies (3 to 7, 11) that strike northeast and
southwest from the historic Tomtebo Mine (Figure 1).
- A total of 26 target zones (1 to 26) have been
identified based on EM or conductive anomalies where 11
target zones are medium priority and three are high priority
(Figure 1 and Table 1).
- A total of 11 target zones (A to K) were identified
based on only magnetic high anomalies where seven target
zones are medium priority and four are high priority (Figure 1 and
Table 2).
- A ground gravity survey over the Tomtebo Mine Trend has been
approved, and is scheduled to commence imminently.
Historic Tomtebo Mine Target
The Tomtebo Mine was picked up as high priority target zone 7
where coincident electromagnetic (EM) and magnetic high responses
have been identified. The EM anomalies are present within the
late time gates, which indicates strong conductivity that likely
correlates with the copper-gold dominant sulphide mineralization at
the mine. Additional EM anomalies are also seen east of the
Tomtebo Mine, and on the flanks of a significant magnetic high
anomaly.
Drill targets have been generated through Maxwell plate modeling
of the EM data at the Tomtebo Mine, which produced three conductive
plates that have a combined strike length of 375 m, thickness of 14 to 78 m, and vertical extent of at least 213 to
600 m. Magnetic modeling within
the Tomtebo Mine Trend produced six magnetic plate targets that
have a combined strike length of 750
m, thickness of 12 to 168 m,
and vertical extent of at least 28 to 356
m.
Historic Lövås Mine Target
The Lövås Mine is within high priority target zone 24, which
comprises a north to south oriented magnetic high feature that is
associated with a limestone/marble unit that has been partially
replaced by iron and polymetallic sulphides. Electromagnetic
(EM) anomalies are also present along three survey lines around the
Lövås Mine with two of the EM anomalies within the significant
north-south magnetic anomaly.
One of the single peak EM anomalies was modeled for drill
targeting, and shows a steeply dipping body of moderate
conductivity with significant thickness. The modeled
conductor has a near surface strike length of 150 m, thickness of 25
m, and vertical extent of at least 300 m.
Skallerberget Target
The high priority Skallerberget target is at the south end of
target zone 24, and comprises a conductive anomaly that is observed
approximately 500 m south of the
Lövås Mine and within the same magnetic high anomaly as
Lövås. The EM anomaly at Skallerberget is weakly to
moderately conductive, and is located proximal to the historic
Skallerberget Iron-Lead Mine.
The EM anomaly at the Skallerberget target has been modeled as a
steeply dipping weak to moderate conductor. The anomaly is a single
peak and is explained by a body with significant thickness.
The modeled conductor has a near surface strike length of
125 m, thickness of 27 m, and vertical extent of at least
200 m.
Källberget Target
The Källberget target is at a medium to high priority that
comprises target zones 21 and 22. Conductive anomalies at
Källberget are seen along a trend that strikes for approximately
700 m. The Swedish Geological
Survey mineral occurrence database reports several historic small
mines and mineral occurrences in the area (Moren 1, 2, 3 and
Flatåsen 4) that are associated with copper- and iron-sulphides.
The EM anomaly trend consists of weakly to moderately conductive
anomalies.
A single EM anomaly was chosen for plate modelling within the
700 m long conductive trend at
Källberget. The trend is expected to be of lower conductivity on
most of the other profiles where it has been defined. The modeled
EM anomaly is explained by a steeply dipping body of moderate
conductivity with a near surface strike length of 200 m, thickness of 30
m, and vertical extent of at least 400 m.
Kvistaberget Target
The medium priority Kvistaberget target comprises target zone
26. Kvistaberget consists of a single peak EM anomaly that is
located on a topographic high. The Swedish Geological Survey
mineral occurrence database reports a historic small mine
(Kvistaberget 4) with copper- and iron-sulphides (chalcopyrite and
pyrrhotite) that is associated with the EM anomaly. There are
several other sulphide occurrences within a few hundred meters of
the Kvistaberget EM anomaly, however, none of them have any
associated EM anomalies. The decay rate for the conductive anomaly
at Kvistaberget indicates moderate conductivity.
The EM anomaly at the Kvistaberget target has been modeled as a
steeply dipping weak to moderate conductor. The data fit is better
for a body with a large down-dip extent, but this parameter is not
well constrained by the data. The modeled conductor has a
near surface strike length of 150 m,
thickness of 20 m, and vertical
extent of at least 400 m.
Next Steps at Tomtebo Property
- Ground gravity survey over the Tomtebo Mine Trend.
- Ongoing interpretation of the geological and geochemical data
obtained from fieldwork conducted at Tomtebo in the fall of
2020.
- Permitting for a Q1 2021 drill program focused on the historic
Tomtebo Mine has commenced.
Table 1: Identified Target Zones Based on EM
Anomalies
Target
Number
|
Ranking
|
Geology
|
EM
response
|
Magnetic
response
|
1
|
Very low
|
Metavolcanics
|
Low-high
|
Low-high
|
2
|
Medium
|
Metavolcanics
|
Low
|
None
|
3
|
Low
|
Metavolcanics
|
High
|
None
|
4
|
Low
|
Metavolcanics
|
High
|
On flank of mag
high
|
5
|
Low
|
Metavolcanics
|
Medium
|
High-medium
|
6
|
Low
|
Metavolcanics
|
High
|
Low
|
7
|
High
|
Metavolcanics
|
High
|
High
|
8
|
Low
|
Metavolcanics
|
Low-high
|
Low
|
9
|
Medium
|
Metavolcanics
|
Low-medium
|
On flank of mag
high
|
10
|
Very low
|
Metavolcanics
|
High
|
Low
|
11
|
Very low
|
Metavolcanics
|
Medium-high
|
Low
|
12
|
Medium
|
Metavolcanics
|
Low-Medium
|
High
|
13
|
Medium
|
Intrusion
|
Low-Medium
|
On flank of mag
high
|
14
|
Medium
|
Intrusion
|
Low
|
On flank of mag
high
|
15
|
Low
|
Metavolcanics
|
Low
|
Low-high
|
16
|
Medium
|
Metavolcanics
|
Low
|
On flank of mag
high
|
17
|
Low
|
Metavolcanics
|
Low
|
Low-high
|
18
|
Medium
|
Metavolcanics
|
Low-medium
|
Low-medium
|
19
|
Medium
|
Metavolcanics
|
Low
|
On flank of mag
high
|
20
|
Low
|
Metavolcanics
|
Medium-high
|
Medium
|
21
|
Medium
|
Metavolcanics
|
Low-high
|
Medium
|
22
|
Medium
|
Metavolcanics
|
Medium-high
|
Low
|
23
|
Low
|
Metavolcanics
|
Low-medium
|
Low
|
24
|
High
|
Metavolcanics
|
Medium
|
High
|
25
|
High
|
Metavolcanics
|
High
|
High
|
26
|
Medium
|
Intrusion
|
Medium
|
On flank of mag
high
|
Table 2: Identified Target Zones Based on Magnetic High
Anomalies
Target
Letter
|
Ranking
|
Geology
|
Mag
response
|
A
|
Medium
|
Metavolcanics
|
High
|
B
|
High
|
Metavolcanics
|
High
|
C
|
Medium
|
Metavolcanics
|
High
|
D
|
Medium
|
Metavolcanics
|
High
|
E
|
High
|
Metavolcanics
|
High
|
F
|
Medium
|
Metavolcanics
|
High
|
G
|
Medium
|
Metavolcanics
|
High
|
H
|
Medium
|
Intrusive
|
High
|
I
|
Medium
|
Basic
metavolcanic
|
High
|
J
|
High
|
Metavolcanics
|
High
|
K
|
High
|
Metavolcanics
|
High
|
Technical Information
All scientific and technical information in this news release
has been prepared by, or approved by Garrett Ainsworth, PGeo,
President and CEO of the Company. Mr. Ainsworth is a
qualified person for the purposes of National Instrument 43-101 -
Standards of Disclosure for Mineral Projects.
About District Metals Corp.
District Metals Corp. is led by industry professionals with a
track record of success in the mining industry. The Company's
mandate is to seek out, explore, and develop prospective mineral
properties through a disciplined science-based approach to create
shareholder value and benefit other stakeholders.
The advanced exploration stage Tomtebo Property, located in the
Bergslagen Mining District of south-central Sweden, is the Company's main focus. The
Tomtebo Property comprises 5,144 ha, and is situated between the
historic Falun Mine and Boliden's Garpenberg Mine located 25 km to
the northwest and southeast, respectively. Two historic
polymetallic mines and numerous polymetallic showings are located
on the Tomtebo Property along an approximate 17 km trend that
exhibits similar geology, structure, alteration and VMS/SedEx style
mineralization as other significant mines within the district.
Mineralization that is open at depth and along strike at the
historic mines on the Tomtebo Property has not been followed-up and
modern systematic exploration has never been conducted on the
Property.
On Behalf of the Board of Directors
"Garrett Ainsworth"
President and Chief Executive Officer
(604) 288-4430
Neither TSX Venture Exchange nor its Regulation Services
Provider (as that term is defined in policies of the TSX Venture
Exchange) accepts responsibility for the adequacy or accuracy of
this release.
Cautionary Statement Regarding "Forward-Looking"
Information.
This news release contains certain statements that may be
considered "forward-looking statements" within the meaning of
applicable securities laws. In some cases, but not necessarily in
all cases, forward-looking information can be identified by the use
of forward-looking terminology such as "plans", "targets",
"expects" or "does not expect", "is expected", "an opportunity
exists", "is positioned", "estimates", "intends", "assumes",
"anticipates" or "does not anticipate" or "believes", or variations
of such words and phrases or state that certain actions, events or
results "may", "could", "would", "might", "will" or "will be
taken", "occur" or "be achieved" and other similar expressions. In
addition, statements in this news release that not historical facts
are forward looking statements including anticipated results of
future exploration and the results of additional compilation
work.
These statements and other forward-looking information are
based on assumptions and estimates that the Company believes are
appropriate and reasonable in the circumstances, , including,
without limitation, assumptions about the reliability of historical
data and the accuracy of publicly reported information regarding
past and historic mines in the Bergslagen District the
Company's ability to raise sufficient capital to fund planned
exploration activities, maintain corporate capacity and satisfy
the exploration expenditure requirements required by the
definitive purchase agreement between the Company and the vendor of
the Tomtebo property (the "Definitive Purchase Agreement") by the
times specified therein (failing which the Tomtebo Property will be
forfeited without any repayment to the Company); and stability in
financial and capital markets.
There can be no assurance that such statements will prove to
be accurate and actual results, and future events could differ
materially from those anticipated in such statements. Important
factors that could cause actual results to differ materially from
the Company's expectations include the risk that historic data
regarding the Tomtebo property is unreliable, the risk that
information concerning production and mineralization at current and
historic mines within the Bergslagen District proves to be
inaccurate; the risk that the Company will be unable to raise
sufficient capital to finance planned exploration (including
incurring prescribed exploration expenditures required by the
Definitive Purchase Agreement, failing which the Tomtebo Property
will be forfeited without any repayment of the purchase price);
future metal prices, general economic, market or business
conditions, and other exploration or other risks detailed herein
and from time to time in the filings made by the Company with
securities regulators, including those described under the heading
"Risks and Uncertainties" in the Company's MD&A for the
financial year ended June 30,
2020. The Company does not undertake to update or revise any
forward-looking statements, except in accordance with applicable
law. Readers are cautioned not to put undue reliance on these
forward-looking statements.
SOURCE District Metals Corp.