World of Investment - Das Finanzportal für Ihren Erfolg an der Börse!

Angeregt durch einen anderen Thread, in dem es um eine Frick Empfehlung ging, hab ich hier vielleicht was für den einen oder anderen.  Ich bin selber mit dabei und konnte schon einiges an Gewinn mitnehmen. 

http://www.globexmining.com/

Das Unternehmen war auf der 1. Rohstoffkonferenz vertreten und wird auch vom Frick in seiner Sonderausgabe der Emailhotline empfohlen. Es handelt sich demnach um ein Explorationskonglomerat und eine Royaltiesgesellschaft mit 75 verschiedenen Projekten über die komplette Rohstoffpalette. 

Scheint also einiges an Potenzial mitzubringen  

Globex Mining klotzt, wo andere kleckern

Globex Mining (WKN: 911 712) - Während die überwiegende Anzahl der Firmen im Rohstoffbereich von einem Tief zum anderen schleicht und nicht so recht auf die Beine kommt, vermeldet die kanadische Explorationscompany Globex Mining eine Privatplatzierung im Millionenbereich. In einem äusserst schwachem Marktumfeld gelang es Globex Minings CEO Jack Stoch 500.000 Aktien seines Unternehmens zu einem Erlös von 2,125 Millionen kanadischen Dollar an den Mann zu bringen. Das alleine stellt bereits eine Leistung im aktuellen Umfeld dar, doch setzte Stoch noch eins drauf: die Ausgabe dieser Aktien erfolgte zu einem Kurs von 4,25 CAD und das sind fast 50% Aufschlag auf den tagesaktuellen Kurs an der TSX! Das zeugt einerseits vom Verhandlungsgeschick Stochs und andererseits vom enormen Vertrauen der Zeichner und der überzeugung, dass Globex zu einer echten Erfolgsgeschichte werden kann. Weitere 450.000 Aktien sollen innerhalb der nächsten beiden Wochen noch ausgegeben werden.

Mit den geplanten Gesamterlösen von 4 Mio. CAD will Stock weiter an der Entwicklung seiner knapp 90 Projekte arbeiten und vor allem sein Magnesium-/Talk-Projekt Deloro voranbringen.

Mit freundlichen Grüßen

Ihr Volker M. Riemer
Chefredakteur
-------------------------------

Rohstoff-Spiegel
c/o Volker M. Riemer
Gänsbichlstraße 5a
A-5400 Hallein
Österreich

Telefon: +43 / 699 / 12 38 03 21
Website: www.r ohstoff-spiegel.de
E-mail: info@rohstoff-spiegel.de

Hinweis gemäß § 34 WpHG (Deutschland):
Mitarbeiter und Redakteure des Rohstoff-Spiegels halten folgende in dieser Ausgabe besprochenen Wertpapiere: KEINE

Hinweis (Österreich):
Die Autoren und Autoren im des Rohstoff-Spiegels legen gemäß § 48f Abs. 5 BörseG offen, dass sie selbst an einzelnen Finanzinstrumenten, die Gegenstand der Analysen sind, ein finanzielles Interesse haben könnten.

Churchill County, Nevada

(Click on property name above to display map)

Property:

Ownership:

Geology:
The property's host rocks are siliceous pyroclastic rhyolites. Two major epithermal quartz-adularia vein systems have been identified on the property. The veins contain gold and silver as electrum and silver as chlorargyrite and argentite. The vein systems on the property cover an area of 0.9 square miles (2.3 km2), of which only 4% has been tested by drilling to an average depth of 25 metres, leaving a large area open to exploration.

A historical mineral resource (non NI-43-101 conformable) stands at 2.1 million tons grading 0.04 ounces per ton gold and 1.2 ounces per ton silver.

Previous Work:
The property was originally staked in 1914. In 1918, Tonopah Mining Co. conducted underground development and sampling with some additional sampling conducted in 1948. A 270-metre long adit was driven in the 1970's.

In 1978, Bell Mountain Mining Co., a subsidiary of American Pyramid Resources Inc., did a substantial underground sampling program including driving the 180-metre Varga adit along the Stockton Vein (Spurr). A comprehensive feasibility study was completed in 1981, which returned positive metallurgical test results. In 1984, Santa Fe Mining Co. drilled 51 reverse circulation holes principally in the Varga area and ten holes in the Sphinx area. Between 1988 and 1993, N.A. Degerstrom drilled 104 holes, completed a technical feasibility study and permitted the property for open-pit mining and heap leaching.

Property:

History: (Hunters Point)

Geology 

General Geology:  The property falls within Precambrian Grenville type rocks consisting of formations of parageneiss, quartzite, granite gneiss and garnet gneiss. The property in a regional sense is on the western outer edge of a large basinal structure which may be a synclinorium.

UTM ZONE 17 - NTS 33D-C-E-F
(click on project name for location map)

Ownership:
In 2000 and 2001, Globex Mining Enterprises Inc. and its partners Aurogin Resources Ltd. and Sparton Resources Inc. acquired 100% interest in 616 cells (map designated claims) covering 35,657 hectares (approximatley 88,108 acres) in the Wemindji area of northwestern Quebec, east of James Bay. The cells were within UTM Zone 17, NTS 33D-C-E-F.

In early 2004, Globex, Aurogin and Sparton optioned the claims to a third party and each retained a 1% Net Diamond Royalty as well as a 1% Net Smelter Royalty on all minerals other than diamonds. Work since 2003 has caused the property to be reduced to 97 cells totalling 4,958.7 hectares which have exploration potential for diamonds and gold.

Regional Geology: The rocks underlying the proposed survey block are Archean in age and belong to the western extension of the La Grande structural sub-province. The La Grande sub-province is a volcano-plutonic belt, composed of 30% gneiss, 10% volcano-sedimentary rocks and 60% granitic plutonic rocks with mafic and ultramafic dykes. Very little geologic mapping has occurred in this region since Remick in 1976 (DP 446).

Structural: There are 3 kimberlite localizing structures intersecting in the Wemindji sector of James Bay Quebec. They are: 1) the Winisk River fault extension in Ontario that becomes the Sakami graben in Quebec; 2) Kapuskasing structural zone; and 3) the Otish lineaments.

1. Kimberlites of the Attawapiskat area are located where the Winisk River fault splays to the East and North, slightly SE of a NE trending Proterozoic diabase dyke.

The Winisk River fault continues its East and Northward migration forming an arcuate, approximately E-W structure and ends up as the Sakami graben in Quebec. This East and Northward arcuate structural pattern is also observed separating the Bienville - La Grande and the Minto - Bienville sub-provinces. The Winisk River fault itself separates the Sachigo and Winisk sub-provinces.

2. The Kapuskasing structural zone extends from south of Lake Superior in the United States, across Ontario, Quebec and up to the Torngat region in the Ungava district.

The Kapuskasing structural zone has both kimberlite and diamond occurrences along its length in Ontario and in the United States, but remains virtually untested in Quebec.

Diamond exploration activity is ongoing on the Kapuskasing structure in particular in the Torngat region of Quebec.

A Ph. D. thesis by Serge Genest, interprets a regional structural element from the Otish up to the east, coast of James Bay.

Points of interest:

All three of these regional possibly diamondiferous kimberlite localizing structures (Winisk River extension/Sakami graben, Kapuskasing structural zone and the Otish lineament), intersect in the vicinity of Wemindji.

In the Attawapiskat area, a third structural element is also involved. It is the Nottaway River - Saguenay Zone.

It is interesting to note that chromium deposits are located on the combined lineaments of Winisk River extension/Sakami graben in both Ontario and Quebec. They are in Ontario, the Bib Trout Lake deposit and in Quebec , the Pro-Or showings. On the Quebec side of the structure, there are also alkaline intrusions. Both chromium deposits and alkaline intrusions are indicative of deep structural breaks as are kimberlites.

Several linear geophysical structures are seen to parallel these diamondiferous structures just south of Wemindji in 33D/15, 16.

History: There is of significant exploration in the area of the properties.

General: Interest in the area has been sparked by the discovery by Majescor Resources of large quantities of "indicator minerals" which are pathfinders for kimberlites and fragments of kimberlite, the host rock for diamond deposits. Indicator minerals are minerals of specific chemical nature, for example G10 garnets, which are most often found in association with diamondiferous kimberlites.

Also, preliminary exploration by Dianor some 100 km to the northeast of the same structural corridor as the Majescor claims has returned zinciferous chromites which are said to have similar chemistry to chromites (as well as at least one micro diamond) found in diamond bearing lamprophyres in the Wawa area.

Globex and its partners, Aurogin and Sparton, originally staked 616 cells (the equivalent of approximately 1,850 standard unsurveyed claims) on specific targets based on structural parameters and geophysical signatures similar to those that could be found associated with kimberlites. Over 75 claim blocks were acquired each covering one or more individual kimberlite targets. 97 of the cells have been renewed following preliminary field work. The bulk of the renewed claims are in areas 33C09, 33C14, 33D16, 33F03, 33F05 and 33F14.

Note: Attached map shows original properties within the immediate area of Wemindji.

Grand Calumet Uranium Fluorite Deposit
Grand Calumet Township, Quebec
NTS 31F/15

Location:
The property consists of 8 claims totalling 354.6 hectares located on lots 28 to 31 Range 7 and lots 30 to 33 Range 6, in Grand Calumet Township, Quebec, approximately 35km northwest of Hull on the Ottawa River and 2km NE of the village of Riviere-Berry.

Ownership:
The property is 100% owned by Globex Mining Enterprises Inc. and was acquired by staking.

Access:
The property is easily accessible via all weather gravel and paved roads.

History:
The property was first worked by Calumet Uranium Mines Ltd. from 1953 to 1954 during which period radiometric surveys, along with stripping and sampling were undertaken following the discovery of significant radioactivity. Based on these surveys and the positive sampling results, diamond drilling was started in the spring of 1954 and by June 1955, 20,082 feet of drilling in 39 holes had been completed.

Diamond drilling and scintillometer surveys showed two important radioactive zones with the most promising area near the intersection of two zones in lots 29 and 30, Range VII.

Further drilling was undertaken in the area with a reported 80 holes being drilled. Geological mapping, mineralogical studies, and further analysis followed with all work being completed by 1956.

Government records do not show any work being submitted since 1956, with the property remaining in the same hands most recently under the name of Albarmont Mines Corporation.

Economic Geology:
There are two main types of mineralization on the property.

The first is characterized by coarse grained and irregularly shaped fluorite- pyroxene skarns. The fluorite is dark purple and commonly contains long narrow prisms of partially altered uranothorite. Dark green pyroxene, apatite, pink calcite, scapolite, feldspar and several other minerals are also present. Associated rocks are well developed pyroxene granites, syenites and hybrids. This type of zone occurs on lots 28 to 31 inclusive, Range 7. Assays up to 4% U3O8 and 20% ThO2 have been recorded from this type of mineralization.

The second is characterized by limestone or skarn composed principally of white to salmon-pink calcite. Small amounts of diopside, lithium bearing yellow mica and chondrodite are also present.

Radioactive minerals include cubes of black uranoan thorianite and grains of red uranothorite. The rock units outcrop in a band which strikes N60BE and dips southeast of the contact between limestones and pyroxenic granites on lots 29 and 30, Range 7.

A radioactive zone extends some 500 feet on surface with a few feet of width exposed. A 1,500 pound bulk sample assayed 0.10% U3O8 and 0.15% ThO2, the radioactive minerals being uranoan, thorianite, uranothorite and monazite. The zone appears to be a calcite rich skarn which closely resembles the limestone in which it occurs. Structurally the area of the zone is complex with folding and cross-folding evident. This zone was reported to contain 490,000 tons averaging 0.05% U3O8 and 0.15% ThO2.

An odd third type of slightly radioactive mineralization occurs on the lot line of lots 28 and 29, Range 7. Here, pits have exposed sulphide rich rock which has weathered to rusty material.

(The above descriptions were paraphrased from Geological Report 80, Radioactive Mineral Occurrences of the Province of Quebec, by D.M. Shaw, 1958, pages 30 to 32 inclusive.)

The only reference to the property subsequent to 1958 is the 1983 Annual Report of Albarmont. Within, their report a possible tonnage of 1,000,000 tonnes grading 0.08% U3O8 , 0.29% ThO2 and 10-15% fluorite is indicated.

Suffield Mine

Ascot Township, Quebec

NTS 21/E5

Property:                    The property is located four miles (6 km) southwest of Sherbrooke, Quebec, Canada and consists of 9 mining claims, covering 617 hectares. 

Ownership:               The property is owned 100% by Globex.

Geology:                     The property is situated on the northwest flank of the overturned Sherbrooke Anticline, which is dissected by series of thrust faults. The area’s two distinctive lithological formations are the felsic to intermediate volcanics and schists of the Ordovician-aged Ascot Formation and, sediments of the Siluro-Devonian-aged Francis Group. Both units are intruded by small ultramafic, granite, diorite and lamprophyre bodies.  The property’s stratigraphic sequence, from west to east, consists of a sedimentary assemblage capped by a  thick sequence of sericite schists and porphyritic rhyolite.

                                     Disseminated and volcanic massive sulfide mineralization occurs at a sediment-volcanic contact. Mineralization consists chiefly of sphalerite and pyrite, with lesser amounts of chalcopyrite and galena. Mineralization appears to be controlled in part by rolls and dips in the contact surface. A sample at the Silver Star Zone assayed 12.5% Cu, 408.1 g/t Ag and 46.3 g/t Au. A mineral resource of 540,000 tonnes grading 7% Zn, 0.9% Cu, 0.5% Pb, 91 g/t Ag and 0.27 g/t Au still exists at the Suffield Mine.

Previous Work:        The claim group contains two past mineral producers (the Suffield King and Howard Mines) and several prospects (the Silver Star, North Howard and No.4 Shaft zones).  The property experienced intermittent mining activities from 1863 to 1956. From 1949 to 1956, Ascot Metals Company developed the Suffield Mine No.3 Shaft.  Production totalled 600,000 tons grading 6.5% zinc, 0.8% copper, 0.45% lead, 2.5 opt silver and 0.007 opt gold. The mine closed prior to the completion of the No.4 Shaft. 

                                     SOQUEM carried out geological, geochemical and geophysical surveys and diamond drilling in 1968 and 1969.  In 1972, Lynx Canada Exploration drilled three short holes which confirmed the Suffield results. In 1985, Copper Stack Resources Ltd. completed geophysics and drill follow-up on the Silver Star zone.  A total of 2,116 feet in six drill holes were put down.  An IP survey was carried out by Spartan Mining Ltd. in 1987. 

                                     The property was optioned in 1989 by Noranda Exploration Company, Ltd., which completed a program of combined geophysical (magnetometer and VLF-EM), geochemical and geological surveying, trenching and diamond drilling for a total of 2,632 metres in 19 drill holes.  During 1990, an additional 1,627 metres of drilling was completed with four drill holes. The Noranda’s drilling encountered significant gold and base metal mineralization.

Glacial moraine covers parts of the area, especially west of the granitic stock.

Molybdenum showings occur along the summit and on the southeast flank of a topographic crest extending towards the northeast of Mount Saint-Sebastien. The zone of interest is 5500 feet long and 1000 feet wide.

The highest point, topographically, is in Gayhurst Township a lot 17, range IX. Its elevation is 2540 feet, which is about 1000 feet above Drolet lake. A good road leads to the entrance of the adit on the east side of the mountain.

In 1962, the name of the company was changed to Copperstream-Frontenac Mines Ltd., and the property was optioned to Molybdenum Corporation of America. Between July 1962 and December 31st, 1963, this company sampled the underground workings and drilled 30 horizontal holes for a total footage of 3000 feet.

In 1963, Molybdenite Corp. of America did a non NI 43-101 resource calculation which reported 2,000,000 tonnes grading 0.50% MoS2.

At the beginning of 1964, Copperstream-Frontenac Mines Ltd. did underground drilling. At the end of the same year Rio Tinto Canadian Exploration Ltd. optioned the property and drilled 17 holes in the South Zone and 3 in the North Zone. In addition, the company bulk sampled 210 feet of the underground workings.

Since 1964, no work has been undertaken on the claims.

Destor Township, Quebec
NTS 32D/10-11
(Click on project name above to display maps)

Property: The Lyndhurst property is located approximately 22 miles (35 km) due north of Rouyn-Noranda, Quebec. There are 88 claims plus one mining concession totalling 1,994 hectares, making up the principal property.

Ownership: