High-level epithermal system. Near-surface gold & silver in jasperoids, with potential for blind polymetallic replacement mineralization.
- October 2016, Prospero signed a Letter of Intent with Pan American Silver allowing PAA to earn in to 80% of El Petate
- Precious metal enhanced possible carbonate-hosted replacement deposit (CRD) proximal to the historic Pachuca-Real del Monte mining district, accessible by road
- Steep and strata-bound jasperoids host near-surface gold & silver mineralization
- Five drill-ready targets; 27 drill sites already permitted with surface-owner permissions granted.
- The significant size of the silicified zones indicates that Petate is a robust mineralized system with excellent potential to host a replacement type deposit at depth with elevated precious metals.
The 6,800 hectare property is located 30km northwest of the historic Pachuca-Real del Monte mining district (Figure 1
), on the western side of the Sierra Madre Oriental fold belt, within a northwest trend of historic deposits including Zimapan (Hidalgo) and La Negra (Queretaro).
Extensive mapping and sampling have defined five key drill-ready targets in the Petate West and Petate East areas. Two targets have anomalous gold grades at surface and are potentially large enough for open pit mining. A drill permit --good for 2 years- was granted on September 7, 2015 covering 27 drill sites. Surface access for these targets has been granted by the land owners.
In April 2017, Prospero secured a C$1.5-million strategic investment from Fortuna Silver Mines Inc -- a growth oriented min-tier silver and gold producer- to fund first-pass, proof of concept drilling on 3 of our key targets, including Santa Maria del Oro.
In addition to drilling, future work should test the potential for blind carbonate-replacement bodies of manto and/or chimney type, containing Ag, Pb, Zn and ± Au similar to the Zimapan or Santa Eulalia polymetallic systems.
Detailed mapping of the property has identified two domains, Petate West (~5 km north-south) and Petate East (~2 km north-south), each with distinct geological and geochemical signatures. Nearly 1,200 rock chip samples have been collected to date in the two zones. Most samples are chip-grab or chip-channel samples between 1 to 1.5m long, or continuous channel samples, sampling outcrops or jasperoid boulders and fragments within float.
In the West zone, multi-gram gold assays were obtained from the the Apartadero, El Tajo and the Petate SW reef. At Petate East, sampling returned multi-ounce silver assays. The Apartadero area (in the Petate West zone) shows stronger gold values associated with Ag-Hg-Sb-As, whereas the Petate East zone is characterized by stronger silver values in association with Au-Ba-Mn.
The presence of low temperature silica invasion and silicification, associated with elevated Hg, Sb, and As indicate that the surface exposures at Petates may correspond to the upper parts of a preserved mineralized system at depth.
The Petate mineral occurrences are hosted in the El Abra limestone of Lower Cretaceous age. These occur in a dome of the Mesozoic fold belt of the Sierra Madre Oriental. Scattered outliers of overlying andesites of the Tertiary Pachuca Group which do not host silicification suggest that the Petate hydrothermal system is more similar in age to the Zimapan skarn/replacement type deposit (~42Ma), than the age of the Pachuca vein deposit (~23 Ma).
Petate West Zone
Petate West hosts numerous silica reefs named --from north to south- La Escoba, Apartadero, El Tajo, Tecolotes, and Petate SW reef (Figures 2, 3
). Some are associated with feldspar porphyry dikes with the same orientation. They feature fine crystalline to cryptocrystalline quartz as stockworks, irregular shaped breccias bodies, and veins, as well as silicification of massive limestones. In general, Petate West has higher gold than silver values.
The reefs are easy to follow at surface because of abundant float boulders and sub-outcrops. The presence of iron and manganese oxides associated with the reefs makes them easily visible on Google Earth and ASTER images.
The Plomosas mine, which exploited high grade Pb-Ag mineralization during the 1940's in the south-central zone, appears to be the south-eastern extension of the Tecolotes reef. Samples from this mine exhibit Pb values in the multi-percent range and silver values in the 30 ppm to 200 ppm range (Figure 6
This target features jasperoid outcrops and float over an area of 1.3km by 200m. It yielded the highest overall gold geochemistry in the Petate claims. Highlights (Figure 5
- gold assays ranging from 1 to 6.6 ppm over a length of 500 meters in the central and southeast extension of the Apartadero target
- silver assays ranging from 2.8 to 31.4 ppm
- multi-elemental geochemistry showing elevated mercury, arsenic and antimony anomalies associated with the precious metals
Trenching and detailed sampling in the Apartadero Central area defined a number of targets including jasperoid breccias with gold values ranging from 1.0 ppm to 5.6 ppm, and a structurally controlled vein target anomalous in silver with values ranging 2.8 to 31.4 ppm (Figure 7
). Several jasperoid breccias bodies at Apartadero SE show anomalous gold with values ranging from 1.0 to 6.6 ppm Au.
El Tajo Target
This zone shows intense silica flooding and abundant float of brecciated jasperoid over 500 meters by 150 meters. Anomalous gold values range from 0.1 ppm to 2.4 ppm, distributed in a half moon configuration and at lower elevations at the northwest end of the El Tajo ridge and target zone (Figure 4
The plan view dimensions of both the Apartadero Central-Apartadero SE, and El Tajo target (500 to 600 metres in length, and 150 to 200 meters wide), and presence of widespread fractions of ppm to multi-ppm Au, indicate there is potential for open pit mineralization in both target zones.
Petate SW Reef
This is a tabular silicified reef which outcrops for 1.2 km along a >3 km long regional-scale range-boundary fault on the southern boundary of an uplifted window of Cretaceous folded sediments (Figure 2
). To the northwest it trends under post-silicification Pachuca Group andesite cover. The reef is anomalous in gold (up to 3.6 ppm), silver (38.9 ppm), Hg (up to 36.4 ppm) Sb (up to 3,690 ppm), As (up to 10,000 ppm), Pb (up to 3,310 ppm), and Zn (up to 6,400 ppm).
Petate East Zone
The Petate East zone is made up of four silica bodies named Petate #1 to Petate #4, all of which occur along a strike length of 2.5km. In contrast to the anomalous gold geochemistry at Apartadero, the Petate East geochemistry shows higher silver levels, particularly in the eastern zone, (Petate # 1, #2, and #3 targets) with silver assays commonly above 25 ppm and up to 140 ppm (Figure 5
). Soil sampling indicates that the Petate #1, and Petate # 2 anomalies are open to the west.
The Petate East zone also shows elevated iron and manganese geochemistry with anomalous values up to double digit percent range. The historic "El Aguila" mine at the southern extension extracted manganese-rich ore from a gossan at the contact with a feldspar porphyry dike (Figure 3
). Two samples from the gossan assayed 345 ppm and 595 ppm silver (Figure 5
), highlighting the presence of high grade silver associated with manganese oxides.
This target is exposed in several outcrops along a small creek for a distance of 50m. Thirteen channel samples returned consistent gold values averaging 0.166 ppm Au (with a high of 0.49 ppm), and 10.4 ppm silver (with a high of 89.4 ppm). Soil sampling shows that the Petate #3 target area extends further to the northwest. A subdued gold anomaly extends an additional 400m to the northwest which is also reflected in mercury and iron geochemistry.
Petate East Soil Sampling
487 soil samples were collected from a grid over the Petate East zone (see news release of Jan 28, 2013). Silver anomalies greater than 5 ppm and up to 52.3 ppm are prominent in the Petate #1 and #2 target areas. The anomalies are open to the west particularly in the western (hangingwall side) of the Petate #2 target where the highest silver values (52.3 ppm, 37.4 ppm, and 19.9 ppm) were obtained (Figure 8
Fluid inclusion results obtained from quartz samples from Petates indicate that the fluids associated with deposition of the quartz were relatively low temperature and salinity (130°C to 230°C; 0-3.0 wt.% NaCl equiv). This in turn suggests that the surface exposures in the project area correspond to the upper parts of a preserved mineralized system at depth.
Additionally, the geochemical signature of the Petate West zone (Au-Ag-Hg-Sb-As) indicates a low-sulfidation system. The Petate East zone geochemistry (Ag-Au-Ba-Fe-Mn) is more indicative of intermediate sulfidation hydrothermalism.
Petate hosts two near-surface exploration targets:
- shallow gold mineralization hosted by steep (and possibly also strata-bound) jasperoids, and;
- shallow silver mineralization hosted by manganese-rich, strata-bound mantos.
There is also potential for deeper chimney-manto bodies with semi-massive base metal sulphides, and silver and gold.
Five zones are drill ready:- Apartadero Central, Apartadero SE, El Tajo, Petate SW reef and Petate #3. The Apartadero Central-Apartadero SE and El Tajo targets are both potential open-pittable gold targets. Additional trenching and channel sampling is required in the Petate # 2 target to provide a better understanding of the length, width and grade of the mineralized zone.
Lead time to drilling should be minimal as a drill permit was granted on September 7, 2015 by the Sub-Delegation of SEMARNAT in Pachuca, Hidalgo. The permit is good for 2 years, and includes 27 drill sites which cover the Apartadero, El Tajo, Tecolotes, and Petate East # 3, #2, and #1 targets. Surface access and drilling permits for these targets have been obtained from surface owners as well.
Prospero is planning for first-pass proof of concept drilling at Petate in mid-2017. Funding has been secured via a strategic investment from Fortuna Silver Mines Inc. which was completed in April 2017.
Future work will also test for the presence of blind carbonate-replacement bodies of manto and/or chimney type, containing Ag, Pb, Zn and ± Au similar to the Zimapan or Santa Eulalia polymetallic systems. In this model, copper may become more enriched at depth as the skarn environment is approached. Jasperoid with comparable silver-rich manganese oxides is seen in the shallow portions of Santa Eulalia and other similar deposits, above the principal silver-zinc-, and lead- -rich, carbonate- replacement chimneys and mantos.