Status: Available for Option


The target at El Batamote is a world-class porphyry copper/molybdenum deposit.

Location and Setting

The Batamote project is located in Northern Sonora, Mexico approximately 25 km north of the La Caridad porphyry Cu-Mo deposit along a district scale structural corridor that is inferred to have localized emplacement of mineralized centers. It is situated within the Cananea-La Caridad porphyry belt and the world class Sonora-Arizona-New Mexico Laramide Porphyry Province. The Exploration consists of three Prospects, El Choclo, Bata Sur and Arreadero.

Land Status

The property consists of three mining concessions La Higuerita 4, La Higuerita 7 and La Higuerita 8 covering a surface area of 5,796 hectares.

Previous Exploration

The area has been explored by various companies since the 1950s. A small mine exploited high grade Cu mineralization in the Bata Sur breccia zone. Peñoles worked the area targeting enrichment blanket mineralization. Teck began working the project in 2010 and performed regional and detailed mapping, grid soil sampling, surface rock sampling, ASD analysis, ground and airborne geophysics and drilling including 10,298 meters in 27 diamond drill holes.


A discrete linear trend of porphyry copper/molybdenum deposits extends from Sacaton in Arizona through Silver Bell and the Pima district to Cananea and La Caridad in Mexico. Deposit clusters along this trend show a remarkably even spacing of 65 to 70 km, except between Cananea and La Caridad which are located approximately 120 km apart. Exploration at El Batamote is based in part on the concept that there may be a third buried copper/molybdenum porphyry deposit located between Cananea and La Caridad.

Structure and Alteration

Basement rocks consist of Precambrian Pinal Schist and associated granite intrusives. The area south and west of the property consists of north trending gravels and volcanic tuffs in basin fill. To the east and north laramide aged volcaniclastic rocks are intruded by a large multiphase intrusive complex (58-53 Ma). In this location north trending Oligocene aged porphyry dikes cut through the system. At the El Choclo prospect a mineralized granodiorite porphyry dike was encountered during drilling. Northeast and northwest trending structures represent a complex structural array which appears to have controlled the emplacement of magmatic and hydrothermal systems. Post mineral extension (Tertiary) consists of at least three events of normal faulting. Which has caused dismemberment, tilting and concealment of the western edge of the hydrothermal system beneath basin fill. The exploration area is marked by widespread alteration. The main and strongest alteration zone is 6 km X 3 km in extent. This alteration is truncated by basin bounding faults and is thought to continue under cover.


The main mineralized targets include El Choclo, Bata Sur and Arreadero all within the strong alteration zone.

At Bata Sur hydrothermal breccia bodies containing Cu values up to 0.65% at surface trend northwest and are roughly 850 X 160 m in areal extent. These breccias contain quartz, carbonate, chlorite, chalcopyrite, pyrite and lessor galena and sphalerite. The brecciated area is associated with a soil anomaly (>345 ppm Cu) and a chargeability anomaly. Four drill holes have cut polymictic breccia containing carbonate-quartz ± chlorite ± fluorite cement and pyrite-chalcopyrite ± galena ± sphalerite. The best drill intercepts include 136 m @ 0.26%Cu and 78 m @ 0.16%Cu and 181 m @ 0.20% Cu.

The Arreadero prospect is characterized by widespread chlorite-biotite-kspar alteration. A large N-S trending soil anomaly contains > 150 ppm Cu and is associated with pyrite-chalcopyrite bearing stockwork over a granodiorite stock. This 53 Ma stock contains biotite-kspar and chlorite-sericite alteration and weak pyrite-chalcopyrite mineralization and is similar in age to the La Caridad porphyry copper system.

A northwest trending 3.3 X 0.65 km Cu soil anomaly (>150 ppm) is associated with a large (3.5 X 2.0 km) quartz-sericite-tourmaline and sericite-chlorite alteration zone and sheeted and stock work veining at El Choclo. Four drill holes intersected mineralized porphyry containing sericite-quartz-chlorite alteration and pyrite-chalcopyrite mineralization influences by multiple hydrothermal events. Mineralization is found in both the porphyry and the host volcaniclastic rocks. The best intercepts include 74 m @ 0.13% Cu, 13m @ 0.25% Cu, 28m @ 0.13% Cu, 22m @ 0.15% Cu, 47m @ 0.21% Cu, 49m @ 0.18% Cu, and 42m @ 0.12% Cu and 33m @ 0.14% Cu.

Conclusions and Recommendations

Drilling and surface work by previous explorers has identified three targets related to porphyry Cu centers, El Choclo, Bata Sur and Arreadero that require additional follow-up work.

The El Choclo target is a dike like mineralized porphyry with a minimum extent of 1 x 0.5km, open to the NNW. The target is associated with quartz-sericite and sericite-chlorite alteration, high density veining and a large Cu soil anomaly. The area NNW of El Choclo has the potential to contain a chalcocite blanket under a leached cap area. Follow up mapping and geochemical and alteration sampling is recommended to define drill targets in the leach cap area. Upon receipt of positive results a series of 4 to 7 drill holes drilled to an approximate depth of 500m is recommended to test for copper deposits beneath the leach cap.

Bata Sur contains two mineralized hydrothermal breccia bodies that may represent a distal feature to a porphyry copper center. Limited drilling resulted in significant copper mineralization in polymictic breccia in four drill holes. The potential to encounter economic grades is high in this structural environment. Further drill testing is recommended at Bata Sur to follow up on the breccia targets. A program consisting of 3 drill holes to a depth of approximately 400 meters is recommended.

The Arreadero target is characterized by Cu bearing stockwork associated with potassic alteration as defined by mapping and geochemistry. Previous work performed on the property should be completely reviewed and geostatistical analyses of soil and drillhole geochemistry performed. Additionally, magnetic modeling should be conducted. Further field work would be based on the results of the recommended office studies but should include mapping to identify stockwork veins and rock and soil sampling to further define the copper anomalies associated with potassic alteration. An IP study in this area is recommended to aid in the placement of future drillholes.