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| ![]() Location Located in Shanxian County, Northwest Henan Province, the region covers the East section of the famous Qinling metallogenic belt; one of the most prolific gold producing regions in China. Xiaoshan is located on the same East-West trending zone as the largest gold mine in the area and on a parallel zone to Silvercorp's multi-million ounce Ying Silver Project located 30 kilometres to the south.Work Program Underground sampling. • Xiaoshan is located on a structural zone parallel to Silvercorp's Ying Silver Project located 30 kilometres to the south. The Xiaoshan and Ying projects demonstrate very similar geological settings, structures, and mineralization styles. • The project consists of two exploration permits, the 17.1 square kilometre (km2) Huluyu permit and the 12 km2 Dafangshan permit, for a total land package of 29.1 km2. • Within the Huluyu permit, thirteen gold and silver veins have been mapped at surface. Sampling by the Henan Nonferrous Exploration and Mining Company from underground workings at Huluyu have returned values ranging from 3.0 g/t to 74.6 g/t gold, 121 g/t to 726 g/t silver, 3% to 29% lead, and 1% to 23% zinc. • Within the Dafangshan permit, 7 gold veins have been mapped at surface that vary in length from 212 m to 772 m with average widths from 0.42 m to 0.65 m and average gold grades from 3.00 g/t to 5.77 g/t. Ownership Minco Mining (China) Corporation, a wholly owned subsidiary of Minco Gold Corporation, has entered into a cooperative joint-venture agreement with Henan Nonferrous Geological Mining Co., Ltd. ("HNGM") to jointly explore and develop the precious and nonferrous resources in the Xiaoshan project area. The project consists of two exploration permits for a total land package of 29.1 square kilometres (km2). Under the terms of the agreement, Minco can earn up to 70% equity interest in Xiaoshan with a total contribution of RMB 35 million (approx US$ 4.57 million). Minco will make an initial payment of RMB 15 million (approx US$ 1.96 million) to secure the exploration permits and fund RMB 20 million (approx US$ 2.61 million) in exploration and development before the end of June, 2009. Background
Geology and Mineralization Xiaoshan sits on a structural zone parallel to Silvercorp's Ying Silver Project located 30 kilometres to the south. The Xiaoshan and Ying projects demonstrate very similar geological settings, structures, and mineralization styles. Regionally, both projects sit on the Southern rim of the North China Craton where the Archean metamorphosed rocks of the Taihua Group are the dominant host for the large gold-silver deposits in the East section of the Qinling belt. Tectonically, the Xiaoshan project area sits at the Xiaoshan uplift block on the Southern rim of the North China Craton. Bedrocks within the two permits are primarily Archean migmatite, schist, and gneiss (Taihua Group) which were intruded by Proterozoic diabase dykes and Mesozoic acidic dykes. Vein-alteration zones in the region are dominantly controlled by N-NW (North-Northwest) and NW-W (Northwest-West) trending faults with the mineral deposit type similar to the mesothermal veins of the Coeur d'Alene District in Idaho, U.S.A.. Huluyu Permit The Huluyu Permit covers 17.1 km2. Host rock for gold and silver mineralization is mainly composed of interbedded chlorite-albite schist, sericite-quartz-albite schist, plagioclase- amphibole schist, and biotite-plagioclase gneiss. At the regional scale, the Taihua Group is dominated with gneiss. Within the Huluyu permit there are three sets of faults trending NW (Northwest), N-NW, and NE (Northeast).
Dafangshan Permit The Dafangshan permit covers 12 km2. In this area, 7 gold veins have been mapped at surface. The mineralization is strata bound and occurs as thin veins. Sampling by the Henan Nonferrous Exploration and Mining Company returned values for veins that vary in length from 212 m to 772 m with average widths from 0.42 m to 0.65 m and average gold grades from 3.00 g/t to 5.77 g/t. Two grab samples returned gold values of 12.8 g/t and 21.7 g/t respectively. | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
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