AQUILA neu in meinem Depot. o. T.
http://www.aquilaresources.com/
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the two: >Streifenkarl ab in den Streifenwagen<
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.  |
Die Ergebnisse stehen noch aus für die übrigen 9 Bohrlöcher, es soll sich nur noch um Tage handeln. . .
Da scheint jemand mehr zu wissen als wir!!!
Zink is back: Aquila Resources sitzt in den Startlöchern
Seit zwei Tagen zieht der Kurs des Zink- und Goldexplorers Aquila Resources wieder an. Die Tatsache, dass dabei in Kanada höhere Preise gezahlt werden als in Deutschland, stimmt Anleger zuversichtlich: Ein kontinuierlich steigender Kurs ist vielen Investoren lieber, als eine durch Börsenbriefe ausgelöste Achterbahnfahrt. Für die nächsten Wochen wurden seitens von Aquila Resources weitere Bohrergebnisse in Aussicht gestellt. Es ist daher gut möglich, dass der neuerliche Kursanstieg bereits ein Vorbote dieser Unternehmensmeldung ist. Der Zeitpunkt für eine solche Mitteilung könnte zudem kaum besser sein: Der Weltmarktpreis für Zink hat sich in den letzten Wochen erholt und notiert nun nur noch knapp fünfzehn Prozent unter den alten Höchstständen vom Mai diesen Jahres, Tendenz weiter steigend. Zudem wird Zink wegen der hohen Nachfrage aus China zunehmend als gutes Investment bezeichnet. Die rasche Erholung nach dem Kurseinbruch im Juni spricht für die Stärke von Zink: “Dem knappen Angebot steht eine starke Nachfrage gegenüber, deswegen ist Zink so interessant”, formulierte es gestern ein Fondsmanager der Deutschen Bank in einem Fernsehinterview. Aquila Resources nimmt aktuell wieder Fahrt auf. Eine nachhaltige Kursentwicklung wäre wohl sehr wünschenswert, doch bieten eventuelle Übertreibungen auch Chancen für Trading-Gewinne.
ORONTO, ONTARIO--(CCNMatthews - July 18, 2006) - AQUILA RESOURCES INC. (TSX VENTURE:AQA - News; FRANKFURT:JM4A - News; "Aquila" or the "Company") is pleased to announce additional results from its ongoing drilling program at the Back Forty VMS gold project in the Upper Peninsula of Michigan, where previous exploration has identified multiple lenses of massive sulfide and associated gold mineralization in an extensively altered sequence of rhyolites, tuffaceous sediments and porphyry intrusives.
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The first five holes of the 2006 program targeted the near surface East End (see press release of June 6, 2006), and the next five holes, reported in this release, targeted expansions of the Tuff Zone, Main Zone and the Deep Copper Zone. An additional ten holes have been submitted for analyses with results pending.
Highlights from the latest drill results include Tuff Zone step outs in LK-79 and LK-80:
- 23m interval of 2.8% Zn in LK-79, including 1.96m (1.39m estimated true width) of 16.4% Zn and 1m (0.71m est. true) of 17.85% Zn.
- 6.2 meters (5.9m est. true) of 18.4% Zn, 2.9 g/t Au, 147.8 g/t Ag, and 6.4% Pb in LK-80.
A 50m step out on the Main Zone in LK-79 returned:
- 8.4m (5.4m est. true) of 13.2% Zn in a broader interval of 41m of 3.3% Zn.
Below the Main Zone in LK-79 a copper rich massive sulfide -- the Deep Copper Zone was encountered returning:
- 45.4 meters (29.2m est. true) of 0.77% Cu and 1.6 g/t Au, including 1.1% Cu and 1.7 g/t Au over 16.5 meters (10.1m est. true).
Gold mineralization distinct from massive sulfides was encountered in LK-79, where altered intrusive porphyry margin returned:
- 4.76 meters (2.9m est. true) of 3.94 g/t Au and 3.68% Zn.
In LK-80, the same porphyry margin returned
- 4.6m (4.4m est. true) of 5.3 g/t Au.
In LK-81, chlorite altered footwall rocks to the Tuff Zone returned:
- 1.5 meters (1.4m est. true) of 6.0 g/t Au, 6.22% Zn, and 299 g/t Ag.
More detailed assay results for these drill holes are presented in the table below.
Aquila Resources Inc. Summary Drill Results July 18, 2006 -------------------------------------------------- All Intervals Est. in Meters True g/t % g/t % % Hole # From To Width Au Zn Ag Cu Pb Description -------------------------------------------------- Chloritic rhyolite LK-77 147.5 153.5 5.4 0.42 1.90 57.30 0.01 0.70 fragmental -------------------------------------------------- includes Chloritic rhyolite 149 150.5 1.35 0.23 2.21 37.90 0.01 0.47 fragmental -------------------------------------------------- Chloritic rhyolite 150.5 152 1.35 0.91 4.99 149.00 0.04 1.90 fragmental -------------------------------------------------- Siliceous tuffaceous LK-78 102.5 129.4 17.3 0.37 0.11 2.64 0.01 0.05 sediments -------------------------------------------------- includes Siliceous tuffaceous sediments/ 128 129 0.65 0.32 1.07 7.70 0.01 0.17 Tuff Zone -------------------------------------------------- Chloritic rhyolite LK-78 180.5 204.9 15.9 0.20 0.57 8.67 0.01 0.24 fragmental -------------------------------------------------- includes Chloritic rhyolite 180.5 184.5 2.6 0.38 1.50 27.80 0.01 0.70 fragmental -------------------------------------------------- Siliceous tuffaceous sediments/ LK-79 147 169.75 16.1 0.62 2.79 29.90 0.03 1.23 Tuff Zone -------------------------------------------------- includes Tuff Zone massive 157.3 158.3 0.71 0.70 15.75 81.00 0.05 3.20 sulfide -------------------------------------------------- Tuff Zone massive 158.3 159.26 0.67 1.14 17.15 146.00 0.19 6.01 sulfide -------------------------------------------------- Tuff Zone massive 167.5 168.75 0.88 1.19 3.84 43.20 0.10 2.22 sulfide -------------------------------------------------- Tuff Zone massive 168.75 169.75 0.71 1.18 17.85 153.00 0.02 10.30 sulfide -------------------------------------------------- Main Zone massive LK-79 267.8 276.2 5.9 0.75 13.22 14.00 0.04 0.54 sulfide -------------------------------------------------- includes Main Zone massive 267.8 269 0.84 1.06 14.30 36.00 0.05 2.38 sulfide -------------------------------------------------- Main Zone massive 269 270.5 1.1 0.83 14.45 16.00 0.03 0.62 sulfide -------------------------------------------------- Main Zone massive 273.5 275 1.1 0.58 29.30 8.00 0.10 0.10 sulfide -------------------------------------------------- Semi-massive sulfide stringer in LK-79 351.8 356.56 2.9 3.95 3.68 4.75 0.06 0.02 rhyolite -------------------------------------------------- includes Semi-massive sulfide stringer in 351.8 353.1 0.8 9.49 6.10 8.00 0.13 0.01 rhyolite -------------------------------------------------- Semi-massive sulfide stringer in 354.8 356.56 1.1 3.33 2.01 5.00 0.02 0.04 rhyolite -------------------------------------------------- Deep Copper LK-79 362.8 408.15 29.2 1.60 0.16 16.20 0.77 0.02 Zone -------------------------------------------------- Deep Copper 365.8 428.96 10.1 1.69 0.12 20.36 1.06 0.02 Zone -------------------------------------------------- Tuff Zone massive LK-80 125.79 132 5.9 2.89 18.39 147.76 0.17 6.36 sulfide -------------------------------------------------- includes Tuff Zone massive 125.79 126.8 0.96 8.33 11.90 164.00 0.67 4.11 sulfide -------------------------------------------------- Tuff Zone massive 126.8 127.8 0.95 3.14 32.00 288.00 0.13 13.00 sulfide -------------------------------------------------- Tuff Zone massive 127.8 128.8 0.95 2.33 25.30 143.00 0.08 6.67 sulfide -------------------------------------------------- Tuff Zone massive 128.8 130.29 1.42 1.53 25.20 190.00 0.02 9.47 sulfide -------------------------------------------------- Sheared, altered rhyolite and porphyry LK-80 206.4 211 4.37 5.34 dike -------------------------------------------------- includes Sheared, altered rhyolite and porphyry 208 211 2.85 6.25 dike -------------------------------------------------- Siliceous tuffaceous LK-81 72.5 86.8 13.6 1.59 0.90 54.34 0.05 0.58 sediments -------------------------------------------------- includes Siliceous tuffaceous sediments/ 85.8 86.8 0.95 6.54 4.40 292.00 0.25 3.28 Tuff Zone -------------------------------------------------- Siliceous tuffaceous sediments/ 86.8 88 1.14 0.42 1.88 25.00 0.03 0.24 Tuff Zone -------------------------------------------------- Chloritic rhyolite LK-81 104.5 106 1.43 5.84 6.22 299.00 0.07 2.43 fragmental -------------------------------------------------- g/t=grams per tonne; Au=gold; Zn=zinc; Ag=silver; Cu=copper; Pb=lead
Results from holes LK-77 through LK-81 continue to expand the known massive sulfide zones and improve the understanding of the geometry and grade distribution within these bodies, as well as in the altered and mineralized host rocks. Multiple intercepts of Au and Zn mineralization in both footwall and hanging wall sequences, and the occurrence of Cu and Au rich massive sulfides beneath the Main Zone, attest to the strength of the mineralized system and potential to expand the mineral resources contained within.
Results of the additional 10 drill holes completed to date will be released as they are received. Sample preparation and analyses continue to be conducted by ALS Chemex Labs in Thunder Bay Ontario and Vancouver BC, on split drill core supplied by Aquila. Standards and blanks are inserted in the sample sequences, and check assays and re-runs are conducted as appropriate. Tom Quigley, P.Geo and President of Aquila, is the 43-101 Qualified Person for the Back Forty project and is responsible for the contents of this press release.
Certain information regarding the Company contained herein may constitute forward-looking statements under applicable securities laws. Such statements are subject to known or unknown risks and uncertainties that may cause actual results to differ materially from those anticipated or implied in the forward-looking statements. The securities being offered have not and will not be registered in the United States under the United States Securities Act of 1933, as amended (the "1933 Act") or any state securities laws, and may not be offered or sold within the United States or to or for the account of benefit of U.S. persons absent U.S. registration or an applicable exemption from U.S. registration requirements. This news release does not constitute an offer to sell or a solicitation of an offer to purchase securities in the United States.
The TSX Venture Exchange has not reviewed and does not accept responsibility for the contents of this release.
Mein Tip Kanada Schlusskurs um 1 CAD und das Hoch wird nicht lange auf sich warten lassen :-)