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Figure 1. Regional metallogenic belts, and Milena position.
Milena, 2010, 15,000 ft
Figure 17. (attribution not available, Catholic Univ.?, Chile)
Figure 16. Digenite/Covellite sulfide rubble sample in Teck’s office on the Milena property. Photo 2010 by S.M. Johnson
Milena’s current 15 square Km (1500 Ha) mineral concessions is available for lease or joint venture (Fig 15). The concessions cover a Miocene porphyry gold-copper system associated with dikes and a hornblende diorite intrusive body.
Figure 12c. MIL-003 no significant mineralization
Figure 12b. MIL-002 strong mineralization throughout
Figure 12a. MIL-001 strong mineralization throughout
Figure 5. Chalcanthite-pyrite breccia pipe rubble at “Old 2010 Chalcanthite roadcut”.
Figure 6. Chalcanthite outcrops and an unknown color anomaly found immediately adjacent to high Cu/Mo grade soil/rock chips.
Figure 7. Altered chalcopyrite-bearing tonalite from MIL-002
Figure 8. Mineralized breccia with porphyry clasts from Chalcanthite area
Figure 9. MIL-002 core photo.
Figure 10. MIL-002 Close up of same interval, note exotic pebble of cpy/cov sulfide…NOT vein filling aggregation
Figure 11. MIL-002 @262m Felsic Dike with sulfide (A-veinlets} with thin reaction rims and quartz bearing semi filled voids.
Figure 2. Milena and the “Flat Plate/Steep Plate” transition zone, (after M. Marot, PhD…undated)
Figure 1. After: Teck, Exploration 2009, F. Daley, VP Exploration Presentation (porphyry model inset from Holliday & Cooke, 2007).
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