Regulus Resources Inc. ("Regulus" or the
"Company", TSX-V: REG, OTCQX: RGLSF) is pleased to
report the results from drill hole AK-21-46 from the AntaKori
copper-gold project in Peru. The goals of this drill hole were to
expand skarn mineralization to the north of existing resources and
provide a better understanding of the geometry of the high-grade
breccia previously encountered at the project. Hole AK-21-46
successfully intercepted an upper zone of skarn mineralization and
the high-grade breccia in multiple intervals. The hole was
terminated in strongly mineralized breccia and porphyry at 1,201.70
m as the drill rig being used reached its maximum depth capacity.
Highlights:
- Intercepted an
upper zone of skarn mineralization retur ning 185.8 m of 0.41%
CuEq
- Intercepted
multiple intervals of high-grade breccia mineralization surrounded
by moderate grades in quartzites crackled by silica-replacements
and sulphide veinlets
- 50.45 m of
2.64% CuEq in high-grade breccia
- 17.25 m of 0.81%
CuEq in crackled quartzite wallrock
- 16.40 m of 0.58%
CuEq in crackled quartzite wallrock
- 5.40 m of 0.73%
CuEq in crackled quartzite wallrock
- 9.90 m of 0.56%
CuEq in crackled quartzite wallrock
- 36.00 m of
1.37% CuEq in high-grade breccia
- Hole ended in this
interval, with the last 11.45 m of the hole averaging 2.13%
CuEq
- The breccia matrix
in this interval is largely composed of mineralized porphyry with
the last 4.4 m of the hole entirely in mineralized porphyry
-
Mineralization remains open in multiple
directions
Dr. Kevin B. Heather, Chief Geological
Officer of Regulus, commented as follows:
“Breccia bodies commonly tend to have irregular
shapes that can range from large pipe-like to dyke-like bodies and
combinations of both within a single system. This breccia body
appears to have aspects of both, and additional drilling will be
required to better define the geometry and size. Having said that,
the fact that we continue to see very high grades within the
breccia where we have intersected it and that it remains open in
multiple directions continues to be encouraging. It is very
uncommon to see continued “crackling” and mineralization in
quartzites, which are notoriously poor host rocks, unless there is
a strong mineralizing system nearby. We know from previously
reported hole AK-18-26 that this breccia has significant size
potential. The fact that AK-21-46 hit two intercepts of the breccia
368.10 m apart, with significant mineralization in between, in poor
host rocks, indicates we may be on the shoulder of a larger system.
The next steps will be to test, in all directions, for potential
extensions and the source of this breccia-style
mineralization.”
John Black, Chief Executive Officer of
Regulus, commented as follows:
“We are very encouraged by the results from
drill hole AK-21-46. The skarn intercept encountered in the upper
portion of the hole will likely increase the size of our current
resource by expanding the conceptual resource pit beyond its
current limits, and by allowing us to capture resource blocks that
were previously outside the conceptual pit and thus unreportable.
More drilling will be required to fully understand the nature and
geometry of the underlying high-grade breccia, but the fact that we
hit multiple intercepts and that the hole ended in very attractive
mineralization is encouraging, considering the size of the target
area and the early-stage of our exploration program at the Anta
Norte targets. We have two rigs turning and look forward to
reporting additional results on a more steady basis throughout the
remainder of this year.”
Table 1 below provides more details on the
mineralized intercepts encountered in AK-21-46. The location of the
reported drill hole is indicated in Figure 1. Figure 2 displays a
cross section of AK-21-46.
Table 1. AntaKori Hole AK-21-46 |
Drill Hole |
Mineralization Style |
From(m) |
To(m) |
Interval (m) |
Cu(%) |
Au (ppm) |
Ag (ppm) |
As (ppm) |
CuEq (%) |
AK-21-046 |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
Interval |
Skarn |
283.30 |
|
469.10 |
|
185.80 |
|
0.23 |
|
0.19 |
|
4.17 |
|
181 |
|
0.40 |
|
including |
Skarn |
283.30 |
|
305.00 |
|
21.70 |
|
0.39 |
|
0.29 |
|
7.38 |
|
174 |
|
0.67 |
|
including |
Skarn |
374.55 |
|
436.60 |
|
62.05 |
|
0.31 |
|
0.29 |
|
5.31 |
|
259 |
|
0.56 |
|
Interval |
Breccia |
771.70 |
|
822.15 |
|
50.45 |
|
1.83 |
|
0.95 |
|
14.66 |
|
1,424 |
|
2.64 |
|
Interval |
Crackled Quartzite |
837.90 |
|
894.70 |
|
56.80 |
|
0.42 |
|
0.10 |
|
5.29 |
|
916 |
|
0.54 |
|
including |
Crackled Quartzite |
846.75 |
|
864.00 |
|
17.25 |
|
0.69 |
|
0.08 |
|
6.58 |
|
1,156 |
|
0.81 |
|
and |
Crackled Quartzite |
874.30 |
|
890.70 |
|
16.40 |
|
0.41 |
|
0.15 |
|
6.47 |
|
1,011 |
|
0.58 |
|
Interval |
Crackled Quartzite |
917.20 |
|
922.60 |
|
5.40 |
|
0.51 |
|
0.26 |
|
4.47 |
|
1,005 |
|
0.73 |
|
Interval |
Crackled Quartzite |
1,070.70 |
|
1,157.05 |
|
86.35 |
|
0.26 |
|
0.03 |
|
1.33 |
|
564 |
|
0.30 |
|
including |
Crackled Quartzite |
1,085.60 |
|
1,095.50 |
|
9.90 |
|
0.52 |
|
0.04 |
|
2.02 |
|
744 |
|
0.56 |
|
Interval |
Breccia/Porphyry |
1,165.70 |
|
1,201.70 |
|
36.00 |
|
1.16 |
|
0.17 |
|
9.64 |
|
3,522 |
|
1.37 |
|
including |
Breccia/Porphyry |
1,190.25 |
|
1,201.70 |
|
11.45 |
|
1.81 |
|
0.24 |
|
16.14 |
|
4,124 |
|
2.13 |
|
The grades are uncut. Cu Eq and Au Eq values were calculated using
copper, gold and silver. Metal prices utilized for the calculations
are Cu – US$2.25/lb, Au – US$1,100/oz, and Ag – US$14/oz. All
intervals presented above consist of sulphide mineralization. No
adjustments were made for recovery as the project is an early-stage
exploration project and metallurgical data to allow for estimation
of recoveries is not yet available. The formulas utilized to
calculate equivalent values are Cu Eq (%) = Cu% + (Au g/t * 0.7130)
+ (Ag g/t * 0.0091). |
Accompanying Video:
Click the following link to watch Dr. Kevin B.
Heather explain the importance of hole AK-21-46 and to view several
photos of the mineralized intervals.
https://youtu.be/_36zY1JGPM4
Discussion of Results:
Drill Hole AK-21-46 was drilled
at an azimuth of 140 degrees and dip of -75 degrees. The location
of the reported drillhole was designed to test for northward
extensions of skarn mineralization and to acquire additional
information on the geometry of the high-grade breccia-style
mineralization discovered in hole AK-18-26, which returned 473.20 m
of 1.39% CuEq hosted in a breccia unit that is open in multiple
directions (see press release dated January 30, 2019).
Drill hole AK-21-46 starts with a thin zone of
Miocene sub-volcanic intrusions to depths of 35 m to 40 m prior to
entering the calcareous Cretaceous sedimentary sequence, with a
well-developed skarn until the basal quartzite at depth. From 128 m
to 210 m the drill hole intercepts a porphyry dyke which is
affected by endoskarn alteration with a weak retrograde overprint
with associated weak disseminations of pyrite and chalcopyrite. The
hole then encountered 80 m of marble with weak retrograde skarn
veins with magnetite-pyrite-chalcopyrite, prior to entering into a
well-developed skarn interval from 290 m to 431 m, with moderate
mineralization occurring as disseminated chalcopyrite-pyrite in
retrograde altered skarn intervals, as well as 1- to 2-metre
intervals of massive magnetite-sulphide horizons, which also carry
gold and silver mineralization.
Fine-grained calcareous sediments (converted to
hornfels) occur from 431 m to 470 m, with skarn development and
associated chalcopyrite-pyrite-magnetite mineralization. Following
the fine-grained sediments, the hole passes into Farrat Formation
quartzites which display minor dissemination of sulphides and
occasional chalcopyrite-pyrite and enargite-tennantite veins.
At 770 m the drill hole encountered a large
breccia body developed in quartzites and cemented by massive
pyrite-chalcopyrite-bornite with a late infilling of
enargite-tennantite, very similar to the mineralization reported in
drill hole AK-18-26. The breccia body is well developed until 822 m
and progressively changes to quartzite wallrock cut by numerous
zones of crackle-breccia exhibiting moderate to weak
bornite-chalcocite-enargite-tennantite ± chalcopyrite
mineralization, before re-entering the well-mineralized breccia
body at 1,165 m until the last few metres of the hole where it
transitioned into a porphyry intrusion body. Of particular
importance is that this lower breccia intercept locally has the
porphyry intrusion as the matrix to the breccia clasts, suggesting
there may be a temporal and possibly a genetic relationship between
the porphyry, the breccia, and the mineralization.
Update on Drilling
Activities:
The Company is currently active with two drill
rigs on the AntaKori project (see Figure 1 for locations). Hole
AK-22-47 is testing the continuity of skarn mineralization observed
in hole AK-19-34 (see press release dated September 5, 2019) and
AK-21-46. As well, AK-22-47 will be drilled on Colquirrumi claims
where the Company has the right to earn up to a 70% interest by
completing 7,500 m of drilling (see press release dated May 18,
2016). The Company had completed 3,669.70 m of drilling on
Colquirrumi claims prior to the start of AK-22-47. Hole AK-22-48 is
testing the northern extension of skarn mineralization observed in
AK-21-46 as well as seeking additional information on the breccia
target. At the time of this release, AK-22-47 was approximately 800
m deep, and AK-22-48 was approximately 1,200 m deep, with both
approaching the operational limit for their respective drill
rigs.
Qualified Person
The scientific and technical data contained in
this news release pertaining to the AntaKori project has been
reviewed and approved by Dr. Kevin B. Heather, Chief Geological
Officer, FAusIMM, who serves as the qualified person (QP) under the
definition of National Instrument 43-101.
ON BEHALF OF THE REGULUS BOARD
(signed) “John Black” John BlackCEO and Director
For further information, please
contact:
Regulus Resources Inc.Phone: +1
604 685-6800Email: info@regulusresources.com
About Regulus Resources Inc. and the
AntaKori Project
Regulus Resources Inc. is an international
mineral exploration company run by an experienced technical and
management team. The principal project held by Regulus is the
AntaKori copper-gold-silver project in northern Peru. The AntaKori
project currently hosts a resource with indicated mineral resources
of 250 million tonnes with a grade of 0.48 % Cu, 0.29 g/t Au and
7.5 g/t Ag and inferred mineral resources of 267 million tonnes
with a grade of 0.41 % Cu, 0.26 g/t Au, and 7.8 g/t Ag (independent
technical report prepared by AMEC Foster Wheeler (Peru) S.A. dated
February 22, 2019, see press release dated March 1, 2019).
Mineralization remains open in most directions.
For further information on Regulus Resources
Inc., please consult our website at www.regulusresources.com.
Sampling and Analytical
Procedures
Regulus follows systematic and rigorous sampling
and analytical protocols which meet and exceed industry standards.
These protocols are summarized below and are available on the
Regulus website at www.regulusresources.com.
All drill holes are diamond core holes with PQ,
HQ or NQ core diameters. Drill core is collected at the drill site
where recovery and RQD (Rock Quality Designation) measurements are
taken before the core is transported by truck to the Regulus core
logging facility in Cajamarca, where it is photographed and
geologically logged. The core is then cut in half with a diamond
saw blade with half the sample retained in the core box for future
reference and the other half placed into a pre-labelled plastic
bag, sealed with a plastic zip tie, and identified with a unique
sample number. The core is typically sampled over a 1 to 2 metre
sample interval unless the geologist determines the presence of an
important geological contact. The bagged samples are then stored in
a secure area pending shipment to a certified laboratory sample
preparation facility. Samples are sent by batch to the ALS
laboratory in Lima for assay. Regulus independently inserts
certified control standards, coarse field blanks, and duplicates
into the sample stream to monitor data quality. These standards are
inserted “blindly” to the laboratory in the sample sequence prior
to departure from the Regulus core storage facilities. At the
laboratory samples are dried, crushed, and pulverized and then
analyzed using a fire assay-AA finish analysis for gold and a full
multi-acid digestion with ICP-AES analysis for other elements.
Samples with results that exceed maximum detection values for gold
are re-analyzed by fire assay with a gravimetric finish and other
elements of interest are re-analyzed using precise ore-grade ICP
analytical techniques.
Neither the 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.
Forward Looking Information
Certain statements regarding Regulus, including
management's assessment of future plans and operations, may
constitute forward-looking statements under applicable securities
laws and necessarily involve known and unknown risks and
uncertainties, most of which are beyond Regulus' control. Often,
but not always, forward-looking statements or information can be
identified by the use of words such as "plans", "expects" or "does
not expect", "is expected", "budget", "scheduled", "estimates",
"forecasts", "intends", "anticipates" or "does not anticipate" or
"believes" or variations of such words and phrases or statements
that certain actions, events or results "may", "could", "would",
"might" or "will" be taken, occur or be achieved.
Specifically, and without limitation, all
statements included in this press release that address activities,
events or developments that Regulus expects or anticipates will or
may occur in the future, including the proposed exploration and
development of the AntaKori project described herein, the
completion of the anticipated drilling program, the completion of
an updated NI 43-101 resource estimate and management's assessment
of future plans and operations and statements with respect to the
completion of the anticipated exploration and development programs,
may constitute forward-looking statements under applicable
securities laws and necessarily involve known and unknown risks and
uncertainties, most of which are beyond Regulus' control. These
risks may cause actual financial and operating results,
performance, levels of activity and achievements to differ
materially from those expressed in, or implied by, such
forward-looking statements. Although Regulus believes that the
expectations represented in such forward-looking statements are
reasonable, there can be no assurance that such expectations will
prove to be correct. The forward-looking statements contained in
this press release are made as of the date hereof and Regulus does
not undertake any obligation to publicly update or revise any
forward-looking statements or information, whether as a result of
new information, future events or otherwise, unless so required by
applicable securities law.
Figure 1 – Plan
Maphttps://www.globenewswire.com/NewsRoom/AttachmentNg/233e0d67-0738-43ae-a962-2e6d7b9bf443
Figure 2 – Cross Section displaying Hole
AK-21-46https://www.globenewswire.com/NewsRoom/AttachmentNg/fb85eaad-2811-4dda-a7d7-8f4329ebec19
Regulus Resources (TSXV:REG)
Historical Stock Chart
Von Nov 2024 bis Dez 2024
Regulus Resources (TSXV:REG)
Historical Stock Chart
Von Dez 2023 bis Dez 2024