| DeerNi copper deposits in the middle of Maqin County ,Qinghai Province Shan southern slope of Deer Ni, Cu, Zn, is a mainly cobalt and other elements can be more comprehensive utilization of the deposit, in the reserves that contain a large (S), four large-scale (Copper, zinc cobalt, gold, selenium), three medium-sized (zinc, silver, cadmium), a small (Ga) a total of nine the number of comprehensive deposit. But also a serpentinite huge reserves can create high-quality FCMP the non-metallic deposit. Before the end of the last century, the deposit is the "stay mine," With the continuous development of the national economy and the improvement of traffic conditions, the current deposit has been listed on the domestic mining companies - Zijin Mining companies use and implementation of mining.As the mine is located in high altitude areas, and because the deposit is in a special geological location, its tectonic setting and structural environment more controversial in recent years as the geological work increased the deposit on a new progress .This article is based on the above topics on the status quo.Papers discussed Deer Ni geological background, with their predecessors DeerNi deposit in the mining area and found the new mining area, the focus at the top of the ore body to a set of sedimentary rocks (iron siliceous slate) for the breakthrough to mine ore with the probe data TYPOMORPHIC other mineral ores compared with the typical deposit at home and abroad compared with pyrrhotite ore body in the distribution of the preliminary study of the genesis. And through the mineralization of the past and prospecting signs summary of the previous mine breccia-serpentinite relations with the ore body, the combination of remote sensing image interpretation of images, data, explore the direction of exploration, the following is the main understanding:1,Animaqing structure through the deposition mélange and ophiolite and tectonic ophiolite in the material composition, output location, structural deformation and comprehensive information on regional structure, stated in the mining area in the middle of a tectonic Mian on the unit is in a slightly - Animaqing structure with the western part of the site.2,.The Deposit through geological features and Fugue on rock mining research, defined the sedimentary rocks for mineralization determine the environment is of great significance. Then the sedimentary rocks and sedimentary rocks outside the mining area compared to identify them as two different elements, different causes of the rock. Ore body at the top of the sedimentary rocks that could be described as containing carbon iron siliceous slate, while the latter known as the carbon content of Al-Si slate. The iron and silica slate at home and abroad typical deposit can be the "iron cherts" Comparative analysis, Al-Fe-Mn triangular diagram, for hydrothermal determine its causes, so as to the causes and Deer Ni deposit process of mineralization Provided important corroboration.3,Through the ore in pyrrhotite, pyrite and sphalerite mineral composition of electronic probe studies, and Kalatongke grams of copper and nickel deposit (pyrrhotite, pyrite), the reactor City Pali Po Mo porphyry deposit (sphalerite, pyrite) components contrast, further confirmed the genesis of the type, and magma from the melting and granite deposits and the hydrothermal deposits are different. Combined with other information that comprehensive study of mineralization Deer Ni deposit has experienced submarine jet - + superposition of the deposition process.Based on this research, comprehensive analysis of information, access to regional metallogenic 4:00 of the understanding, summing up the seven signs prospecting, exploration to the future direction of the two.
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