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Gallardo Project

Precious Metal: Gold-Silver, Copper, Gypsum

Owner: Exploradora Rios de Cobre
Location: Agua Prieta, Sonora, Mexico

Information Available:

Geology: Yes Drilling: No
Geochemistry: Yes Reserves: No
Geophysics: Yes Other: No

Land Tenure:

Owned (100%)

4 Concession, exploration

4,490 hectares

Surface Rights Secured: No

Agreement Type Sought: Lease/Option

Property Summary:

Property consists of the Gallardo Concession and fractions, a 7 km x 7.5 km area in Sonora, Mexico, adjoining the Arizona border from 10 to 17 km east of Agua Prieta. Title to the concession is expected in early 1999. Valid prior interior concessions cover part of an active gypsum mine, a gypsum prospect, and a gold prospect. The remainder is exploration concession E-82/20867 covering 4,490 hectares.

The paved highway from Agua Prieta to Chihuahua crosses the property. An improved gravel road linking Agua Prieta to Rusbayo crosses the Cenizas Mountains somewhat south of the property. Numerous ranch roads provide interior access to the property. Ranches on the western side of the property are served with electrical power. Topography is generally flat at elevation 1,300 m except for isolated peaks rising to about 1,600 m. Vegetation is typical of the chaparal zone of the Sonoran Desert: cactus and mesquite predominate. Surface water flows only intermittantly during strong rainfall.

Geology Summary:

A large Tertiary epithermal gold system is present, based on local gold-bearing, pyritic, hydrothermal breccias, abundant quartz-chalcedony-calcite fracture fillings, widespread silicification of structural intersections and permeable units, and general  pyritization of rocks in a 4 x 7 km area. Anomalous gold and trace element geochemistry accompanies brecciation and silicification.

Oldest exposed rocks are recrystallized limestones and siltstones of the Cretaceous Bisbee Group. The carbonate beds are preferentially silicified and intruded by quartz monzonite porphyry north of a major east-west structural zone. A thick Paleozoic carbonate section probably underlies Cretaceous rocks. Jurassic intrusions, volcanic rocks, and structures may also occur at depth in the property. The Bisbee porphyry copper of Jurassic age is located 50 km northwest of the property. Principal host rocks to gold mineralization are a west-dipping sequence of volcaniclastic beds, andesite tuffs, and rhyolite tuffs that unconformably overlie Cretaceous rocks and appear to be intruded by a pyritic rhyolite plug or sill. A strong north-trending shear zone more than 1,000 m wide cuts the entire section and is associated with alteration and gold mineralization at intersections of E-W, N60E, and N50W veinlets in a generally continuous zone 5 km long.

Gallardo is comparable to the Sleeper mine gold deposit in Nevada, based on comparable length and width of structural intersections in similar Mesozoic sedimentary rocks overlain by Tertiary felsic volcanic units. Gold mineralization at both locations is principally related to hydrothermal breccias at structural intersections in Tertiary volcanic units. Sleeper is famous for its bonanza electrum ore shoots in younger breccias surrounded by a broad area of fracture-hosted gold, arsenic, and antimony mineralization. Initial Sleeper reserves were 3.4 Mt grading 7.5 g/t gold and 27.4 g/t Ag. At Gallardo, permeable unwelded tuffs and volcaniclastic beds are widely altered, silicified, and weakly mineralized, suggesting that bulk-tonnage disseminated gold mineralization may also be present.

Geochemistry Summary:

Thirty-five rock chip samples from outlying alteration occurrences average 0.017 ppm gold with a highest value of 0.180 ppm.  Silver averages 0.62 ppm with a highest value of 7.3 ppm.  Arsenic averages 34 ppm with a highest value of 207 ppm.  Barium averages 1005 ppm with a highest value of 14,600 ppm. Visible barite is seen in many samples and has been mined from thick veins near hydrothermal breccias.  Galena is seen in samples with the higher gold results.   Results for approximately seventy additional samples are available upon request.

Geophysics Summary:

Gallardo is situated on the prominent N50E trending zone of gravity anomalies that includes the Bacoachi and Arizpe base and precious metal mineral districts in Sonora and the Hachita porphyry copper system in New Mexico. Additional information will be reported in the near future.

Drilling Summary:

None

Reserves Summary

None

Other:

None

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DISCLAIMER: MineMarket.com, its affiliates, associates, or assigns are not responsible for the content, accuracy or marketability of any of the services or information contained in or linked to this website. Furthermore, MineMarket.com, its affiliates and its assigns make no representation or warranty of any kind or character with respect to the adequacy of any services or information contained in or linked to this website for any purpose and disclaim all liability of any kind arising from its use.