Regional Mineralisation Pattern of the Eastern Beishan Orogenic Belt,Inner Mongolia

The eastern section of the Beishan Orogenic Belt, located in the western part of the Inner Mongolia Autonomous Region, has favourable metallogenic conditions and rich mineral resources. Through the systematic study of the geological conditions of mineralisation in the area, research on the division of metallogenic units and the law of mineralisation has been carried out, which points out the direction for the next step of the regional mineral search work. The study shows that on the basis of the previous metallogenic unit division, combined with the latest comprehensive metallogenic information, the eastern section of the Beishan metallogenic belt can be further divided into the Yueyashan-Xichangjing gold, copper, chromium and nickel metallogenic prospect, the Hutoushan tungsten, molybdenum, zinc and gold metallogenic prospect, the Suosuojing iron, copper, gold, lead and zinc metallogenic prospect, and the Pantuoshan-Laodonggou gold-antimony, tungsten-molybdenum and lead-zinc metallogenic prospect. Lead-zinc mineralisation prospect.Summarised the regional metallogenic law, in terms of timing, the main metallogenic period is mainly for the Paleozoic era, secondarily Cambrian; from space, gold, tungsten and other minerals are mainly around the Pantuoshan, Wangxushan yingzuihongshan and other important mineralisation rock body internal and contact zone distribution, while the tectonic control effect is obvious, manganese, vanadium and other sedimentary minerals are mainly along the important sedimentary interface distribution.