Equitas Resources Corp. Commences Exploration Program at their Cajueiro Gold Property in Brazil Vancouver, British Columbia, May 9, 2016 – Equitas Resources Corp. (“Equitas” or the “Company”) (TSXV: EQT) (US: EQTRF) (Frankfurt: T6UN) is pleased to announce that exploration at the Cajuiero Project (“Cajueiro”) has commenced. Equitas would also like to report further technical details at Cajueiro, located within the Mato Grosso and Para states of Central Brazil. Summary: The exploration program will focus on expanding and identifying additional mineral resources in the Baldo Target Area (“Baldo”) at Cajueiro. Baldo is host to widespread gold mineralization, and a virtually untested mineralized structural corridor delineated over an 820m strike length on surface. An exploration program targeting the structure has commenced, and will include diamond drilling, trenching and bulk sampling. Chris Harris, President and CEO, stated “Having closed the acquisition we are now focused on moving towards expansion of our flagship Cajuiero resources. We have just started our exploration program which is focused on the prospective oxide zones. When considering the high grade results achieved from surface sampling over the last 18 months, we have identified solid potential to add quality resources to the project.” Technical Update: The Cajueiro Project is located in the Alta Floresta - Juruena Gold Belt, a Proterozoic arc consisting of calc-alkaline granite-volcanic, and medium to high grade metamorphic crustal segments. Historic gold production in the belt is generally recognized to be in the range of 7-10 Moz, primarily from Garimpeiro activity. At Cajueiro, microgranites and rhyolites host a set of Northeast (NE) and East-West (E-W) conjugate shears exhibiting late brittle deformation. These were the primary structural controllers of hydrothermal alteration and associated gold mineralizing processes. Gold and pyrite in the bedrock sulphide domain is contained within hydrothermal alteration envelopes within and adjacent the structures. An alteration assemblage of sericite-epidote- chlorite-quartz readily distinguishes the prospective “green” rhyolite and microgranite from their unaltered reddish counterparts. Observations indicate the quartz veining and related gold-pyrite mineralization to be a late brittle event of the process.
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16-05-09 Equitas Commences Exploration Program at Cajueiro
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Equitas Resources Corp. Commences Exploration Program at their
Cajueiro Gold Property in Brazil
Vancouver, British Columbia, May 9, 2016 – Equitas Resources Corp. (“Equitas” or the
“Company”) (TSXV: EQT) (US: EQTRF) (Frankfurt: T6UN) is pleased to announce that
exploration at the Cajuiero Project (“Cajueiro”) has commenced. Equitas would also like to
report further technical details at Cajueiro, located within the Mato Grosso and Para states of
Central Brazil.
Summary:
The exploration program will focus on expanding and identifying additional mineral resources in
the Baldo Target Area (“Baldo”) at Cajueiro. Baldo is host to widespread gold mineralization,
and a virtually untested mineralized structural corridor delineated over an 820m strike length on
surface. An exploration program targeting the structure has commenced, and will include
diamond drilling, trenching and bulk sampling.
Chris Harris, President and CEO, stated “Having closed the acquisition we are now focused on
moving towards expansion of our flagship Cajuiero resources. We have just started our
exploration program which is focused on the prospective oxide zones. When considering the
high grade results achieved from surface sampling over the last 18 months, we have identified
solid potential to add quality resources to the project.”
Technical Update:
The Cajueiro Project is located in the Alta Floresta - Juruena Gold Belt, a Proterozoic arc
consisting of calc-alkaline granite-volcanic, and medium to high grade metamorphic crustal
segments. Historic gold production in the belt is generally recognized to be in the range of 7-10
Moz, primarily from Garimpeiro activity. At Cajueiro, microgranites and rhyolites host a set of
Northeast (NE) and East-West (E-W) conjugate shears exhibiting late brittle deformation. These
were the primary structural controllers of hydrothermal alteration and associated gold
mineralizing processes.
Gold and pyrite in the bedrock sulphide domain is contained within hydrothermal alteration
envelopes within and adjacent the structures. An alteration assemblage of sericite-epidote-
chlorite-quartz readily distinguishes the prospective “green” rhyolite and microgranite from their
unaltered reddish counterparts. Observations indicate the quartz veining and related gold-pyrite
mineralization to be a late brittle event of the process.
Figure 1: Equitas properties in Brazil
Gold is also present in the saprolite overlying bedrock, in the oxidized equivalent of the sulphide
alteration assemblage. Prospective saprolite hosts an assemblage of sericite-chlorite-silica, with
disseminated limonite and “box-works” of limonite with rare occurrences of chalcopyrite. This
package is clearly visible on surface in many locations throughout the property.
The current Inferred Resource estimates at Baldo (Gustavson 2016) are as follows:
Baldo Sulphide (bedrock)
Baldo Oxide (saprolite)
Inferred
Inferred
Cutoff Tonnes Au Oz Au
Cutoff Tonnes Au Oz Au
g/t (000s) g/t (000s)
g/t (000s) g/t (000s)
0.3 1,108 0.872 31.1
0.3 309 3.029 30.1
0.25 1,319 0.777 33
0.25 309 3.029 30.1
0.2 1,500 0.711 34.3
0.2 309 3.021 30
Figure 2: Property Geology after Chapleau Resources Limited (2007)
Surface sampling at Baldo by ECI Exploration and Mining Inc. (ECI), the former owner of
Cajueiro, in 2012 collected a total of 34 grab samples of the saprolite. Values obtained by
Inductively Coupled Plasma – Optical Emission Spectroscopy (ICP-OES) for these samples
range between 0.01 g/t Au to 118.47 g/t Au, with twenty samples returning values > 0.5 g/t Au,
and an average for the 34 samples of 14.67 g/t Au.
During 2014-15, Alta Floresta Gold conducted geological mapping and prospecting,
supplemented with test pits and trenching, at the Baldo target. This work identified a prospective
NE trending set of structures, up to a combined 25m in width (Figure 2). This target has been
traced over an 820m strike length on surface. At the southern end of this structural corridor, two
randomly selected circa 1 tonne samples of saprolite were taken from two separate test pits. The
samples were split manually and quartered, with an equivalent amount from each pile included in
the samples sent to SGS Laboratories in Belo Horizonte, Brazil for Flame Atomic Absorption
(FAA) analysis. Results are listed in Table 1 (all coordinates listed in WGS 1984, UTM Zone
21S).
TYPE GPS Coordinates
WGS 84, Zone 21S
Sample ID Au g/t
SMP 548267E / 8964740N RR1BDO 5.77
SMP 548261E / 8964661N RCF1BDO 87.20
Table 1
Four bulk samples of saprolite were recently extracted via a backhoe excavator from Baldo, and
processed through an H3 hammer mill. This hammer mill is limited in its milling capacity owing
to the internal grid apertures and will only mill to a maximum particle size of 1.5mm (not
sufficient to liberate a significant portion of the free gold). However, these samples have each
still recovered impressive gold value results, as documented in Table 2.
Tonnes Grams Gold Recovered
5.63 9.90
12.70 17.60
49.00 33.71
22.00 28.82
Table 2
Additional testing at Baldo by Alta Floresta Gold included collection of a 100kg sample of
saprolite, taken across a horizontal length of 2 meters at a depth of 5 meters in a trench (548319E
/ 8964366N). Sample M-1 (see figure 3) was sent for bench-scale metallurgical testing to SGS
Geosol and Minproces in Chile. Sample treatment included chemical analysis, grinding kinetics,
microscopy, diagnostic test leaching and flotation. Analytical results for ICP-OES analysis of the