VANCOUVER, BC,
April 7, 2022 Zacapa
Resources (TSXV: ZACA) (OTCQB: ZACAF) (DE: BH0) is pleased
to announce that the first four holes (RT-21-001 and RT-22-002
through RT-22-004) have cut porphyry style alteration and veining
with multiple intervals containing visible copper minerals and
further expanding the volume of hydrothermal alteration at Red Top
to vertical depths of more than 800 metres. A fifth drill hole is
underway with a planned depth of 1,200 metres to explore deeper
portions of the 100% owned Red Top porphyry copper project in the
Superior Mining District, Arizona.
Drill holes RT-21-001, RT-22-002, RT-22-003 and RT-22-004 were
designed to test the copper potential at depth beneath a >3.5
kilometre by 1.5 kilometre outcropping quartz-sericite-pyrite
alteration zone with a core of advanced argillic alteration
(pyrophyllite-illite-sericite) (Figure 1). Similar to the
previously released drill holes (RT-21-001, RT-22-002, and
RT-22-003), RT-22-004 cut a series of texturally distinct
hypabyssal quartz feldspar porphyry intrusions and importantly
diabase intrusions with varying intensities of porphyry related
hydrothermal alteration (quartz-sericite-pyrite and possibly
sericite-chlorite after biotite), porphyry style "A-Veins",
porphyry style "B-Veins" and intermittent intervals containing
chalcopyrite and bornite mineralization commonly associated with
what appear to be late-stage, open space quartz veins (Figure
2).
Highlights:
- Porphyry style alteration, veining and mineralization has
been confirmed with diamond drilling over an area measuring 1,200
meters by 800 meters and over a vertical extent of over 800 meters
increasing Zacapa's confidence that a significant hydrothermal
system is present and has the potential to host significant copper
mineralization.
- In addition to the large volume of alteration, numerous
favourable host rock lithologies are present including at least
three phases of texturally distinct hypabyssal quartz-feldspar (+/-
hornblende) porphyry intrusions and importantly iron-rich diabase
intrusions which are a key high grade host rock at the nearby (8
kilometers) Rio Tinto/BHP Resolution mine development project (1.8
Bt @ 1.5% Cu)2,4.
- Zacapa is leveraging recently collected airborne (MobileMT)
and magnetic geophysical survey to help vector toward a potentially
higher temperature, more intensely altered copper-rich core to this
newly identified porphyry system in the prolific Superior Mining
District of Arizona.
- Drill hole number five (RT-22-005) is a near vertical hole
situated between drill holes RT-21-001 and RT-22-003 and is
currently at 604 metres depth.
"We are very pleased by the ongoing drill success at Red Top and
the further expansion of a new porphyry footprint in one of the
world's top porphyry copper districts. The geological context
and geometry of the target area are coming into focus and we look
forward to establishing Red Top as a premier copper exploration
project," comments Adam Melnik,
Chief Executive Officer. "Zacapa is incorporating the newly
acquired geophysical data along with more detailed mapping and
remote sensing to assist us in vectoring toward the core of a new
copper-molybdenum porphyry system in Arizona."
Diamond drill holes RT-21-001 through RT-22-004 contain
pervasive alteration of varying intensity and intermittent copper,
gold, and base metal mineralization in favourable host rocks
including multiphase porphyritic intrusions, schist, and diabase
intrusions confirmed by diamond drilling over an area measuring
1,200 by 800 meters and to a depth of more than 800 meters from
surface. Alteration mineral assemblages including
quartz-sericite-pyrite and chlorite-sericite (after biotite) in
diamond drilling and pyrophyllite-illite-sericite exposed at
surface together with mineralization including vein-controlled
chalcopyrite, galena, and sphalerite suggest the first four holes
have tested geology either above or lateral to a copper bearing
"core" in an idealized porphyry system (Figure 4). Surface
mapping and historical Induced Polarization geophysics suggest that
the Red Top system is tilted moderately toward the east suggesting
that the system plunges moderately toward the west (see Figure
4). Ongoing exploration targeting at Red Top will leverage
new geological information collected in the first four drill holes
as well as newly acquired magnetic and electromagnetic data from
the recently completed MobileMT survey to vector toward a potential
copper-rich core to this system which may be located lateral to the
west of the current drill holes or deeper in the system (Figure
4).
Drill Hole Descriptions
Drill Hole RT-22-003
Drill hole RT-22-003 was collared 360 metres north of RT-21-001
and drilled to a total depth of 986 meters (Table 1). The
hole was drilled to expand Zacapa's understanding of alteration and
mineral zonation within the newly identified hydrothermal system
and assist in vectoring toward the associated porphyry center.
RT-22-003 cut a series of granitic porphyry intrusions with
variable phenocryst abundances and sizes hosted by a
quartz-monzonite micro-porphyry. The granite porphyry is
characterized by a weak but pervasive sericite+/-chlorite
alteration mineral assemblage. Sericite and chlorite are present as
vein halos, ranging from 0.1-3 cm in width, and are common
throughout the drillhole cutting all porphyry rocks. Below 811
metres, much of the quartz-monzonite and other porphyritic
intrusions contain patchy to pervasive albitization of feldspar
phenocryst. Sulphide mineralization in RT-22-003 includes vein
hosted pyrite ± chalcopyrite ± bornite ± sphalerite ± galena,
fracture filling pyrite, and disseminated magnetite ± pyrite.
Except for magnetite, mineralization is spatially associated with
veins and intervals of increased vein density.
Drill Hole RT-22-004
Diamond drillhole RT-22-004 (Table 1) was collared 650 metres
north of RT-22-003 and oriented to test an Induced Polarization
chargeability geophysical anomaly by drilling to the west-northwest
from an area of high to low chargeability. RT-22-004 intersected a
thin interval of Pinal Schist cut by a coarse-grained granodiorite
porphyry at 24 metres depth. Below 24 metres the hole intersected
alternating layers of dark, fine- to medium-grained diabase and
granodiorite. From 437 to 623 metres (EOH), the dominant lithology
is a pink to greyish-pink granite porphyry. Intense
alteration/mineralization was present within the Pinal schist and granodiorite porphyry from
11-150 metres including locally over 20 percent pyrite. The
alternating sequence of diabase-granodiorite are present to 437
metres depth and contain weak chlorite and sericite alteration.
Sericite altered plagioclase phenocrysts and magnetite-chlorite
altered biotite is common through much of the granite porphyry
intersected in latter portion of the drillhole. Chlorite-sericite
alteration is also present as vein halos and sericite increases to
a pervasive overprint of the porphyry groundmass where veining is
most abundant. Sulphide mineralization in RT-22-004 comprises
vein hosted pyrite ± chalcopyrite ± bornite ± sphalerite ± galena
and disseminated magnetite ± pyrite. Magnetite is present in all
lithologies and tends to occur as small veinlets and as
disseminations.
DRILL HOLE
ID
|
EASTING
|
NORTHING
|
ELEVATION
(m)
|
AZIMUTH
(°)
|
INCLINATION
(°)
|
PLANNED DEPTH
(m)
|
FINAL DEPTH
(m)
|
RT-21-001
|
489107
|
3692695
|
1,063
|
60
|
-60
|
800
|
1,042
|
RT-22-002
|
489588
|
3692518
|
1,098
|
60
|
-75
|
800
|
779
|
RT-22-003
|
488970
|
3693022
|
1,060
|
90
|
-65
|
800
|
986
|
RT-21-004
|
489034
|
3693577
|
1,100
|
275
|
-60
|
500
|
623
|
RT-22-005
|
489002
|
3692896
|
1,070
|
275
|
-80
|
1,200
|
Ongoing
|
Table 1 – Red Top
drill hole collar information
|
Airborne MobileMT Geophysics
Geophysical Interpretation and Targeting
Expert Geophysics Limited ("EGL") conducted a helicopter-borne
MobileMT electromagnetic and magnetic survey over Red Top in late
February 2022. The objective of the survey was to collect
apparent magnetic, conductivity and resistivity data to aid in the
three-dimensional targeting and geological modeling of the Red Top
porphyry center in the subsurface (Figure 2). Systematic
modeling of these data are ongoing however, interpretation of
2-dimensional products has highlighted a total magnetic intensity,
apparent conductivity and resistivity features of interest
including a coincident magnetic low to high transition interpreted
to represent magnetite destruction (Figure 2B), a resistivity low reflecting alteration or a
buried intrusion (Figure 2D) and an apparent conductivity high
which may represent the presence of sulphide minerals associated
with alteration or mineralization (Figure 2C). These
geophysical features together are considered a high priority
anomaly and potential new drill target.
Survey Parameters
The MobileMT electromagnetic and magnetic survey at Red Top
consisted of four production flights covering 199 line-kilometers
of survey data over a 73 sq km area. The survey lines were oriented
E-W (90°N) at 400 metre spacing, with tie lines oriented
perpendicular to the survey lines and spaced at 4,000 metres.
About the Red Top Porphyry Copper Project
The Red Top porphyry copper project is located in the Superior
Mining District, 8 kilometres northwest of the Rio Tinto and BHP's
Resolution mine development project and approximately 11 kilometres
from the Carlota and Pinto Valley mining operations. Red Top is
comprised of 431 unpatented mining claims covering 8,377 acres. The
Red Top project area exhibits widespread porphyry style alteration
with locally intense alteration spanning approximately 3.5
kilometres by 1.5 kilometres near Red Top hill. These intensely
altered areas of quartz-sericite, as well as zones of pyrophyllite
and illite are analogous to assemblages associated with
mineralization at the upper levels of the Resolution
deposit2,3. This alteration and mineralization at Red
Top are interpreted as the expression of the upper levels of a now
moderately tilted porphyry system that has only seen limited
historical exploration and no previous drilling within the target
area. Zacapa is one of the only exploration companies drilling for
porphyry copper in southeast Arizona, which is dominated by Freeport, BHP and Rio Tinto.
About Zacapa Resources
Zacapa is a copper and gold focused mineral exploration company
engaged in responsible exploration for the new energy economy. Its
projects are concentrated in world class jurisdictions in the
southwest U.S., including Arizona,
Nevada, and Idaho. The
portfolio includes porphyry copper projects at Red Top, Pearl, and
Dewdrop Moon, and epithermal gold projects at South Bullfrog and
Miller Mountain. These assets are
being advanced by a highly disciplined and seasoned professional
team with successful track records of discovery, resource
development and mine permitting.
References
1 Alteration and sulphide
mineralogy has been determined visually from drill core and
confirmed where possible using Portable XRF ("pXRF") and short-wave
infrared (SWIR) analytical devices. Petrographic samples have
been collected and will be used expand upon visual
observations.
2 References to other mines and deposits
made in this news release provide context for the Red Top Project,
which occurs in a similar geologic setting, but this is not
necessarily indicative that Red Top hosts similar grades and
tonnages of mineralization.
3 Manske, S.L., and Paul, A.H., 2002,
Geology of a major new porphyry copper center in the Superior
(Pioneer) district, Arizona: Economic Geology, v. 97, no. 2, p.
197-220.
4 Rio Tinto, 2020, Annual Report
5 Lowell, J.D. and Guilbert, J.M. (1970)
Lateral and Vertical Alteration-Mineralization Zoning in Porphyry
Ore Deposits. Economic Geology, 65, 373-408.
|
Qualified Person
Daniel MacNeil, P.Geo, a
Qualified Person as defined by National Instrument 43-101, has read
and approved all technical and scientific information related to
Red Top contained in this news release. Mr. MacNeil is at
Technical Advisor to Zacapa Resources and has verified the data
disclosed in this press release, including the sampling,
analytical and test data underlying the information.
For more information, please visit www.zacaparesources.com. All
documents are available on Zacapa's profile page on SEDAR at
www.sedar.com.
On behalf of the Board of Directors,
"Adam Melnik"
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 release.
Forward Looking Statements – Certain information set forth in
this news release may contain forward-looking statements that
involve substantial known and unknown risks and
uncertainties. All statements within, other than statements
of historical fact, are to be considered forward looking. Although
Zacapa believes the expectations expressed in such forward-looking
statements are based on reasonable assumptions, such statements are
not guarantees of future performance and actual results or
developments may differ materially from those in forward-looking
statements. Zacapa 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 Zacapa's
control. 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. Readers are advised to rely on their
own evaluation of such uncertainties. Except as required under
applicable securities legislation, Zacapa undertakes no obligation
to publicly update or revise forward-looking
information.
SOURCE Zacapa Resources