ROUYN-NORANDA, QC, June 22, 2021 /CNW Telbec/ - X-Terra Resources
Inc. (TSXV: XTT) (FRANKFURT: XTR) ("X-Terra") is
pleased to announce a drilling update regarding its ongoing drill
program at the Troilus East property located in the James Bay region in the province of
Quebec.
X-Terra has completed five of the planned 12 diamond drill
holes. The five holes, which ranged from 150 to 200 metres in depth
are positioned along the high priority anomaly located on the
southwest grid pictured below.
X-Terra is also excited to announce the preliminary observations
from the drill core.
The program was designed to focus around a strong
1-kilometre-long chargeability anomaly, exhibiting an apparent
width of between 200 metres and 400 metres. It straddles an area
which was difficult to explore and only had limited surface work
due to poor outcropping conditions.
The drill grid corresponds to the south-west part of the "Smoke"
target. Previous prospecting and soil sampling works gave strong
proximity indicator of a mineralized system at about
three kilometres directly south-east of the former Troilus
open pit. The new system identified covers a strike length of
approximately two kilometres where polymetallic sulfides
occurrences were sporadically sampled. X-Terra noted that sporadic
samples over this area returned copper grades up to 0.25%
Cu, silver grades up to 8.0 g/t Ag, zinc grades up
to 0.7% Zn and 0.11 g/t Au, or 0.43g/t
AuEq (see X-Terra press release dated August 13, 2020).
Michael Ferreira, President and
Chief Executive Officer of X-Terra states: "The first
observations of drill core are extremely encouraging, as they are
clearly demonstrating that mineralized outcrops and boulders
could correspond to the extensive sulfides bearing drill core where
varied amounts of polymetallic sulfides (chalcopyrite and
sphalerite) can be observed ranging from one metre to over ten
metre intervals".
X-Terra wants to highlight that copper and silver grades from
drill results recently disclosed by Troilus Gold Corp (TLG) in its
press release dated June 6, 2021, are
in the same range as these first surface results obtained from the
Smoke target. In addition, the host rocks, alteration and
mineralization style are also considered similar (please see
Troilus Gold Corp's press release dated September 10, 2019).
Troilus Gold Corp has recently increased the mineral resources
to 4.91 million AuEq ounces in indicated resources and 3.15 million
AuEq ounces in inferred category (Source: Troilus Gold Corp.
Technical Report on the Troilus Gold-Copper Project mineral
resources estimate, Quebec,
Canada, RPA, dated December 20,
2019. See Troilus Gold Corp's press release dated
July 28, 2020). This information is
strictly for deposit model comparisons and does not imply X-Terra's
Troilus East property may host similar quantities of
mineralization.
Observation summary
The drill grid crosscut an important lithological sequence. This
sequence highlights a progression starting at the north-west side
by andesitic flows interlayered with more felsic brecciated flows,
which comes in contact with a ten-to-twenty-metre layer of felsic
tuffs or sediments, which is locally graphitic. The sequence is
intruded by a mafic intrusion marked by continuous composition
variations from andesite, quartz rich gabbro to a more mafic
counterpart.
Structurally, even preliminary, the whole sequence could be
interpreted as folded with a sheared and faulted contact. The fine
grain and laminated felsic units acting as a non competent layer
molding the mafic unit to create a structural doming effect. Strong
ductile deformation associated with a shear band overprints the
contact, evolving to a tectonic breccia in the more fragile felsic
unit.
The drill grid has yet to cover the entirety of the alteration
system which spans approximately the entire width of the
chargeability anomaly. The combination of alteration minerals
observed includes biotite, muscovite, tremolite, sericite, garnet
and aluminous silicate which is concentrated in bands of a few
metres, distributed throughout complex assemblages indicating
superimposition of events or zoning patterns.
Mineralization
Disseminated iron sulfides (pyrrhotite and pyrite) are common
throughout drill intervals in varied lithological and alteration
contexts. Chalcopyrite and sphalerite are also noted in intervals
ranging from 5 to 20 metres.
Overall, the intermediate volcanics can be considered as the
main host rock for the polymetallic sulfides, presenting as
stringers, laminations, disseminated clots in contact with
centimetric quartz veins or fractures. In addition, foliated and
biotite rich altered gabbro also hosts significant amount of
disseminated pyrrhotite, reaching locally 10% in association with
trace amounts of chalcopyrite.
Close to the fault system, pyrite bearing quartz and
quartz-feldspar veins reaching up to one metre appear, where
variably altered volcanic host rocks become more deformed,
laminated to brecciated.
The following intervals are preliminary and reflect sulfides
concentrations, mostly where chalcopyrite mineralization was
observed, or where obvious vein networks were intersected.
Observations are from holes TESW-21-01, TESW-21-03, TESW-21-04,
TESW-21-07 which were readily accessible at X-Terra's core shack
facility.
X-Terra believes it provides initial validation of the
perspectivity of the high priority anomaly at Troilus East, readers
are strongly cautioned that the information in this press release
is of a preliminary nature and the visual mineralization observed
has not yet been assayed. Also, the intensity of visual
mineralization should not be used to estimate grade of commercial
viability at this stage.
DDH
|
Position
|
From_(m)
|
To_(m)
|
Mineralization
features
|
TESW-21-
01
|
IP Line 9, north-
east limit of the
grid,
|
78
|
89.5
|
10% grey quartz
veins, locally brecciated
and discordant, associated with pyrite
stringers. Hosted in biotite-muscovite-
pyrrhotite rich volcanic host rock.
|
TESW-21-
03
|
IP Line 6, center
of
the grid
|
0
|
3
|
Sulfides rich
lamination in felsic tuff with
pyrrhotite-pyrite-chalcopyrite.
|
TESW-21-
03
|
IP Line 6, center
of
the grid
|
75
|
79.5
|
3 to 5% disseminated
chalcopyrite in a
silicified matrix.
|
TESW-21-
03
|
IP Line 6, center
of
the grid
|
122
|
144
|
3 to 10% disseminated
pyrrhotite with
traces of chalcopyrite. Disseminated in
amphibolitized gabbro.
|
TESW-21-
04
|
IP Line 6, center
of
the grid
|
1.5
|
8
|
2-5% disseminated
polymetallic sulfides
grains and clusters (pyrrhotite,
chalcopyrite).
|
TESW-21-
04
|
IP Line 6, center
of
the grid
|
55
|
85
|
Pyrrhotite
(variable), pyrite, secondary
magnetite, traces of chalcopyrite in
amphibolitized gabbro, local quartz-
feldspar veins (70 to 70.5m).
|
TESW-21-
04
|
IP Line 6, center
of
the grid
|
135
|
150
|
Chalcopyrite
stringers (traces) with
disseminated pyrrhotite and pyrite. Hosted
in sediments and mafic volcanics.
Quartz-carbonate
breccia with quartz
veining from 142m to 144.5m.
|
TESW-21-
07
|
IP Line 9,
southwestern
extension of the
grid
|
15
|
35
|
3 to 10% disseminated
pyrrhotite in a biotite
rich foliated gabbro. Quartz veins stringer
from 32 to 35 metres.
|
TESW-21-
07
|
IP Line 9,
southwestern
extension of the
grid
|
76
|
92,5
|
5 to 10%
pyrite-sphalerite in stringers
associated with a strong shear zone and
partial tectonic brecciation. Alteration
environment dominated by biotite-feldspar.
|
Qualified Person
Jeannot Théberge, P. Geo registered in the Provinces of
Quebec and New-Brunswick, a consultant to X-Terra, a
qualified person under National Instrument 43–101
Standards of Disclosure for Mineral Projects
("NI 43-101"), has reviewed the technical
contents of this news release and has approved the disclosure of
the technical information contained herein.
Forward-Looking Statements
This news release contains statements that may constitute
"forward-looking information" within the meaning of applicable
Canadian securities legislation. Forward-looking information may
include, among others, statements regarding the future plans,
costs, objectives or performance of X-Terra, or the assumptions
underlying any of the foregoing. In this news release, words such
as "may", "would", "could", "will", "likely", "believe", "expect",
"anticipate", "intend", "plan", "estimate" and similar words and
the negative form thereof are used to identify forward-looking
statements. Forward-looking statements should not be read as
guarantees of future performance or results, and will not
necessarily be accurate indications of whether, or the times at or
by which, such future performance will be achieved. No assurance
can be given that any events anticipated by the forward-looking
information will transpire or occur, including the exploration
programs and development (including any drilling programs) of the
Troilus East property, or if it does so, what benefits X-Terra will
derive from the Troilus East property. Forward-looking information
is based on information available at the time and/or management's
good-faith belief with respect to future events and are subject to
known or unknown risks, uncertainties, assumptions and other
unpredictable factors, many of which are beyond X-Terra's control.
These risks, uncertainties and assumptions include, but are not
limited to, those described under "Financial Instruments" and "Risk
and Uncertainties in X-Terra's Annual Report for the fiscal year
ended December 31, 2020, a copy of
which is available on SEDAR at www.sedar.com and could cause actual
events or results to differ materially from those projected in any
forward-looking statements. X-Terra does not intend, nor does
X-Terra undertake any obligation, to update or revise any
forward-looking information contained in this news release to
reflect subsequent information, events or circumstances or
otherwise, except if required by applicable laws.
About X-Terra Resources Inc.
X-Terra is a resource company focused on acquiring and exploring
precious metals properties in Canada.
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 the release.
SOURCE X-Terra Resources Inc.