| The tectonic location of the study area is the middle part of the Sichuan Yunnan north-south structural belt,the west side of Anning River fault zone and the eastern side of the Panzhihua fault.The regional large faults provide abundant material sources for this area.The Qing Gang village of Baima V-Ti magnetite ore section of Tian Ping geological characteristics are systematically studied,the study area of ore bearing rock for early Variscan magmatic rock,orebody in Whitehorse BASIC-ULTRABASIC layered rock mass in the lower part,and the causes of the geological characteristics of ore district for analysis of this type of deposit is of important practical meaning.According to the basic data of 2010 Sichuan provincial geological prospecting fund project in 2011 with the central geological prospecting fund project,through field geological investigation,geophysical prospecting,drilling,method of sample analysis,collecting fully absorbing the previous research results,through 2010 and 2011 deep drilling work,the main conclusions are as follows:The main lithology of the deep ore bearing strata in the ore body is the same as the shallow part,and the content of the main mineral composition is basically the same.The shape of the ore body is in accordance with the ore bearing layer.The ore body moves toward the north and south,tilting to the West or North West,and the dip angle is 60~70 degrees,and the shallow ore body becomes steepening.The genetic type of the deposit is an early magmatic deposit. |
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