Geophysical Program Completed, Drilling Underway HALIFAX, April 13 /CNW/ - Erdene Gold Inc. (TSXV:ERD) today announced it has completed the first phase of exploration at its Zuun Mod porphyry copper-molybdenum project in Mongolia and has initiated drilling. The property is located less than 200 kilometres from the Chinese border, where rail and high voltage power generation facilities are being constructed to service the Jiaguan Iron and Steel complex located in China's Gansu Province. The facilities are being built to source raw materials from Mongolia's Gobi desert region. The recently completed geophysical and geologic mapping program built on previous exploration to provide much more detailed information on structure, alteration and lithological distribution. Geomaster Ltd. has completed a 112-line kilometre gradient and a 20-line kilometre, 200-metre dipole-dipole survey over a four-kilometre by seven-kilometre portion of the Zuun Mod property. It is apparent from the new survey data that the geophysical data and interpretation will result in improved drill hole target selection. Initial areas to be drill tested are located in the southeastern half of the Zuun Mod complex and include the Racetrack Zone, the Stockwork Zone and the Intersection Zone (see maps at www.Erdene.com). The Racetrack Zone: The "Racetrack" occupies the central portion of an elongate stockwork - alteration zone, anchored to the southwest by the Stockwork Zone and to the northeast by the Intersection Zone. A strong copper-in-soil anomaly covers the entire area locally exceeding 500 ppm. The Racetrack is characterized by a quartz ring, which has a saucer-like profile with a diameter of approximately 300 metres. It is believed to represent a vein system related to radial fractures or remnant of a quartz cap. Structures resembling unidirectional solidification textures (UST) and a zone of vuggy quartz are present within the structure, which has an argillic and pyritized granosyenite at its core. The ring is coincident with an area of moderate to high gradient and also a dipole-dipole chargeability anomaly. The nearest hole (KKMD-08, Gallant Minerals/WMC, 2003), approximately 200 metres west, was intensely mineralized from 88 metres to the end of the hole at 279 metres, averaging 530 ppm molybdenum and 560 ppm copper with strong secondary biotite, magnetite clots and locally 100% of the core replaced by K-spar flooding. The Stockwork Zone: Located approximately 1.2 kilometres south of the Racetrack, the Stockwork Zone is characterized by local intense quartz stockwork and sheeted vein systems within biotite granodiorite and granosyenite with copper and molybdenum mineralization related to the veins. The stockwork zone occurs within a broad area of high chargeability and moderate-low resistivity. Previous drilling in the area (Gallant Minerals/WMC, 2003) included hole KKMD-03 which returned two intervals of 38 metres each that average 0.1% molybdenum with 0.46 to 0.49 ppm rhenium. Weaker copper mineralization is also present with a few isolated intervals (two metres) in the 0.25% to 0.61% range. The nearest hole, 500 metres west returned wide sections of highly anomalous copper and molybdenum while no drilling has been undertaken to the south or east where the target area continues under Cretaceous and recent cover. The Intersection Zone: It is apparent from the mapping that there is a strong structural control to both intrusion emplacement and subsequent alteration dominated by quartz-sericite-pyrite (QSP). The three dominant structural systems are; NE-SW, NW-SE, and E-W. The NE and NW systems are interpreted as a conjugate set likely related to near N-S compression, whereas the E-W system appears to be later and superimposed resulting in an intense fracture-cleavage in some places. It is apparent from the preferred NE and NW orientation of QSP-altered zones that mineralized fluids were focused within these fracture systems. This is also inferred by the fact that the best- mineralized holes (3, 4, 5, 7, 13, 14) are situated within these trends. It is significant that these structures intersect in an untested area and that the copper and molybdenum in rock geochemical results in this zone are coincidently anomalous. Summary: -------- Previous exploration of the Zuun Mod prospect outlined an extensive area of hydrothermal alteration and mineralization with distinct copper-molybdenum zones surrounded by large areas of 2% to 5% disseminated and veinlet pyrite. Although the outcrop is somewhat poor, a core area measuring four kilometres by one kilometre was outlined that had intensely altered (quartz-sericite- pyrite) biotite granite/granodiorite porphyry with local stockwork quartz-sulfide veining and UST's. Thirteen widely spaced and relatively shallow holes averaging 250 metres indicate the potential for very significant volumes of mineralization in strongly altered (potassic characterized by abundant secondary biotite) andesitic wallrocks and argillic to weak sericitic in the intrusive rocks. Mineralization ranges from potentially ore grade molybdenum/rhenium/copper mineralization in the Stockwork zone (KKMD-03) to wide, low grade copper zones north of the intersection zone in the 0.1% to 0.2% range with up to several hundred ppm molybdenum. The initial drill program is planned to include a minimum of six holes averaging a depth of 400 metres each. Qualified Person This press release has been prepared under the supervision of Michael Corey, P.Geo., who serves as the qualified person under National Instrument 43-101. All samples are assayed at SGS Laboratory in Ulaanbaatar, Mongolia. In addition to SGS Laboratory internal checks, Erdene Gold incorporates a QA/QC sample protocol utilizing prepared standards, sample splits and duplicates. About Erdene Gold Inc. Erdene Gold Inc. is a mineral exploration company focused on Mongolia with over 20 precious and base metal projects that include 47 licences covering in excess of 840,000 hectares, as well as 19 uranium licences and applications covering more than 1.1 million hectares. Erdene is well funded with a working capital position of approximately CDN$7.6 million. Erdene has 26,232,135 common shares issued and outstanding and a fully diluted share position of 30,828,910 common shares. Erdene Gold Inc. trades on the TSX Venture Exchange under the symbol ERD. Forward-Looking Statements Certain information regarding the Company contained herein may constitute forward-looking statements within the meaning of applicable securities laws. Forward-looking statements may include estimates, plans, expectations, opinions, forecasts, projections, guidance or other statements that are not statements of fact. Although the Company believes that the expectations reflected in such forward-looking statements are reasonable, it can give no assurance that such expectations will prove to have been correct. The Company cautions that actual performance will be affected by a number of factors, many of which are beyond the Company's control, and that future events and results may vary substantially from what the Company currently foresees. Factors that could cause actual results to differ materially from those in forward-looking statements include market prices, exploitation and exploration results, continued availability of capital and financing and general economic, market or business conditions. The Company's forward-looking statements are expressly qualified in their entirety by this cautionary statement. The information contained herein is stated as of the current date and subject to change after that date. Erdene disclaims any intention to update or revise this statement of forward-looking information, whether as a result of new information, future events or otherwise. For additional information visit Erdene's website at www.erdene.com or contact the company via email at info(at)erdene.com. The TSX Venture Exchange has not reviewed and does not accept responsibility for the adequacy or accuracy of this news release.
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