Fitzroy Minerals Exploration Update, Caballos Copper Project, Chile
In the southern half of the Caballos concession, mapping and sampling has identified a large copper-oxide-stained felsic intrusion out-crop associated with the Pocuro Fault, and a set of polymetallic veins to the west. The felsic intrusion is approximately 500 m long by 70 m wide and trend north-south along the fault. A grab rock sample from this intrusion take by the Project QP returned 2.11% Cu, 1.10 g/t Au and 22 g/t Ag (Figure 1). The polymetallic veins to the west are visible in an extensive area approximately 2.0 x 1.2 km. The mineral assemblage in the vein sets is frequently quartz-galena-sphalerite-pyrite with minor chalcopyrite. Assay results from 94 samples in the southern half of the Caballos concession are pending.
Highlights:
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Mineralised intrusions and old workings along the Pocuro Fault Zone host copper mineralisation.
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Grab rock chip samples up to 2.46% Cu in old workings located in a 1.3 km-long dioritic stock.
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New, large (500 m x 70 m) copper-oxide-stained felsic intrusion identified in south Caballos with a grab rock sample grading 2.11% Cu, 1.10 g/t Au, and 22 g/t Ag.
Merlin Marr-Johnson, President and CEO of Fitzroy Minerals commented, "Mapping at Caballos confirms mineralisation along the Pocuro Fault Zone corridor, highlighted by positive results and the presence of old workings. There is a clear association of copper mineralisation with felsic and dioritic intrusions in the main Pocuro Fault corridor at the Project. Three new veinlet-bearing dioritic stocks ranging from 600 to 1,300-m long were identified in the northern part of the Project. The most recent discovery of a large, copper-stained felsic intrusion and the extensive polymetallic veins sets in the southern sector are yet more signals that we are mapping out an extensive mineral system. The plan is to map out the extent of the mineralised intrusions and nearby veins that are associated with the main north-south structures."
Caballos Copper Project, Chile
At Caballos, mapping and sampling was carried out in April and May-June. In April, the focus was on the northern part of the main Pocuro Fault Zone accessed via the Rio Sobrante valley. In May-June, the focus was on the southern part of the PFZ accessed via the Rio Alicahue valley. As of 14 June, 94 grab rock chip samples from the southern area have been collected and sent to the laboratory for analysis with assay results pending. A preliminary Property-scale geological map is provided in Figure 1.
Figure 1. Caballos Copper Project, rock chip sampling geochemistry and geology |
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Assay results have been returned from the 83 northern area grab rock chip samples. Of the 83 samples, 29 samples had values above 0.1% Cu, 18 of the samples had values above 0.5% Cu, of which seven were above 1.0% Cu with a maximum of 2.46% Cu. Gold values between 0.13 and 0.36 g/t Au accompany copper in two of the intrusive stocks. Separately, gold grades up to 1.37 g/t Au, are associated with gossanised zones in volcanic or intrusive rocks.
Copper mineralisation is mostly associated with felsic intrusions (disseminated sulphide-oxide mineralisation) and dioritic intrusions (fracture and vein-related mineralisation) along the main PFZ. Copper oxides are prevalent on fractures, particularly on the contacts between the intrusive bodies and the host rocks.
Old workings are evident close to the northern boundary in an altered dioritic stock that has a mapped extent of 1,300 metres. Copper oxide staining is evident on the edges of the intrusion in fracture planes and vein sets. Four samples from this intrusive, spaced 400 m apart returned values between 0.87% Cu and 2.46% Cu.
Mapping to date has confirmed the PFZ as a structural corridor orientated roughly north-south. The host lithology is predominantly andesitic volcanic rocks to the west, with largely unmineralized tuffs located east of the PFZ. The PFZ structural corridor features dioritic and feldspathic porphyry intrusions into the andesites, frequently elongated and aligned north-south. The contacts are often sheared with minor breccia development. A subordinate southwest-northeast fracture system has influenced the shape of the intrusions and controlled some of the veining.
Zones of weak-intermediate argillic and quartz-sericite alteration feature in some sectors of the feldspathic and dioritic porphyry bodies accompany copper mineralisation. The alteration and the copper mineralisation in the mapped area is concentrated in and/or on contact zones around the intrusions.
The team is focusing on the PFZ which runs approximately north-south across the western portion of the Caballos concession area (Figure 1). Prior exploration also identified hydrothermal breccias with copper, zinc, and local molybdenum in the southern part of the concession area along the PFZ. Recent mapping by Fitzroy Minerals has identified a mineralized felsic intrusion that extends approximately 500 m north-south within a hydrothermal breccia zone of 1.2 km along the PFZ. The felsic intrusion has copper-oxide staining along the majority of its width, with fresh disseminated chalcopyrite occasionally visible. A grab rock sample taken by QP Scott Jobin-Bevans from this intrusion in April returned 2.11% Cu and 1.10 g/t Au.
When geological maps and assays from the southern portion are returned Fitzroy Minerals will undertake a review of the data prior to announcing future exploration plans at Caballos.
QA/QC and Rock Sampling
A total of 177 grab rock chip samples, 163 from outcrops and 3 from small fist-sized pebbles, were collected as part of the geological mapping program (83 from the north and 94 from the south), with chip samples limited to vein widths and up to 2 m-long. The 177 samples collected by the Company and the one (1) grab sample collected by the QP were analyzed by Andes Analytical Assay (AAA) based in Santiago, Chile, using ICP for 31 elements, including copper and silver, and AAS for gold. ICP copper results >10,000 ppm were re-analyzed using AAS and report as total copper (CuT). For the QA/QC, in addition to the standards and blanks used by the laboratory, the Company inserted nine (9) blanks into the sample stream, along with one field duplicate sample. Rock grab samples are selective by nature and values reported may not represent the true grade or style of mineralization across the Property.
Grant of Options
The Company also announces that it has granted 550,000 options (each, an "Option") to purchase up to 550,000 common shares to an officer and certain consultants of the Company under the Company's 10% rolling stock option plan (the "Plan"). The Options are exercisable at the price of $0.15 per common share until XX, 2029, subject to any earlier termination in accordance with the Plan and the requirements of the TSX-V. All Options vested immediately on the date of grant.
Qualified Person
Scott Jobin-Bevans, Ph.D., P. Geo., a Qualified Person as defined by National Instrument 43-101, has reviewed and verified the technical information provided in this news release.
About Fitzroy Minerals
Fitzroy Minerals is focused on exploring and developing mineral assets with substantial upside potential in the Americas. The Company's current property portfolio includes the Caballos Copper and Polimet Gold-Copper-Silver projects located in the Valparaiso Region, Chile and the Taquetren Gold project located in Rio Negro, Argentina, as well as the Cariboo project in British Columbia, Canada. Fitzroy Minerals' shares are listed on the TSX Venture Exchange under the symbol FTZ and on the OTCQB under the symbol FTZFF.
On behalf of Fitzroy Minerals Inc.
Merlin Marr-Johnson
President and CEO
For further information, please contact:
Merlin Marr-Johnson
mmj@fitzroyminerals.com
+1 604-505-4554
For more information on Fitzroy Minerals, please visit the Company's website: www.fitzroyminerals.com
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