Hier der neue Link zur aktuellen Homepage:
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www.aquilaresources.com/
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gestern von www.stock-report.net zu 47 cents ins musterdepot aufgenommen! das depot ist noch ziemlich neu, aber die jungs haben es echt drauf
hier der beweis:

| LK Massive Sulfide, Michigan U.S. |
| The Back Forty Project is an advanced stage exploration program focusing on gold and massive sulfide targets in early Proterozoic rocks in Michigan’s Upper Peninsula. Early in 2002, drill testing of a geophysical anomaly resulted in the discovery of the LK Massive Sulfide. Subsequent drilling in 2003 has defined three lenses of stacked zinc and gold rich massive sulfide mineralization, stringer zone gold mineralization, and adjacent gold rich sections low in sulfides. The LK massive sulfide lenses have excellent exploration potential for expansion and the discovery of additional massive sulfides and low sulfide gold zones. There are also untested airborne and ground geophysical targets, identified from an airborne survey flown over the project area. GEOLOGIC SETTING AND MINERALIZATION The Back Forty Project area is located in Menominee County, Michigan in early Proterozoic (Penokean) aged volcanic rocks of the Wisconsin Volcanic Terrain, an Island Arc sequence of dominantly volcanic and intrusive rocks hosting significant volcanogenic massive sulfide (VMS) deposits and occurrences. The project area consists of a large area centered on the LK massive sulfide, which is hosted by felsic volcanic rocks, siliceous tuffaceous sediments, and younger intrusive porphyries. Massive sulfide mineralization (>80% sulfide largely pyrite and sphalerite) is localized along two stratigraphic horizons (the Main Zone and the Tuff Zone) within a large felsic volcanic center dominated by intensely sericitized and silicified quartz-feldspar rhyolite crystal tuffs. The massive sulfide bodies are enveloped by large stringer-stockwork zones (20-80% sulfide, pyrite+chlacopyrite+sphalerite). Significant precious metal values occur within the massive sulfides and in subjacent stringer sulfides and altered host rocks. The deposit has been folded and tectonically thickened in the core and south limb of a large-scale, west plunging anticline creating a pinch and swell geometry. Faulting has offset portions of the deposit. The massive sulfide lenses show impressive widths and potential continuity. Table I shows a variety of massive sulfide intercepts from both horizons. Table I. Selected massive sulfide intercepts with metal grades. EXPLORATION POTENTIAL Massive Sulfides Potential to expand the existing massive sulfide zones is excellent. The Main Zone massive sulfides remain open down plunge to the west, and ground geophysical surveys indicate probable extension in this direction for at least an additional 425m. The Tuff Zone massive sulfide is open at depth and along strike to the east, and has not been drilled along its surface projection where there is potential for enriched gossans similar to the East Zone. A GEOTEM airborne EM and magnetic survey was flown over the entire project area and has indicated a number of conductive responses potentially caused by sulfide mineralization. Limited ground geophysical follow up on three of these targets indicates coincident gravity and EM responses, further enhancing this potential. Gold Mineralization Impressive gold intercepts in a variety of host rocks peripheral to massive sulfide mineralization suggest strong potential for “gold only” style mineralization. Table II summarizes some of these results. The fact that these intercepts were random “hits” in holes targeting massive sulfide mineralization suggests good potential for expansion. Table II. Host rocks and gold intercepts peripheral to massive sulfide zones. ![]() |
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