The western region has a vast area, a long geological history, and complex tectonic evolution. Under different geological conditions and metallogenic geological conditions, different ages and types of iron deposits have been formed. In addition to the typical ferrosilicon construction, the Anshan iron ore mine has not been discovered at present, all of the country's iron ore processing equipment types have output. Since iron ore deposits in this area are mainly volcanic rocks, deposits are deteriorating, and skarns are the main types of iron deposits, and the harmful components—sulfur exceeds the industrial requirements, it is necessary to carry out beneficiation operations. The co-elevated components in the deposit include copper, lead, zinc, nickel, cobalt and manganese. The iron ore deposits closely related to the hydrothermal activities of the same sedimentary fault often produce the phenomenon of “copper under the upper ironâ€. The similarities between the mineral processing equipment of the Jingtieshan birchgou iron-copper ore, the Mengku iron ore, and the Yamansu iron ore mine have similar phenomena. .
(3) The distribution of spatial distribution is partially concentrated.
The iron ore processing equipment in the western region is consistent with the distribution of the orogenic belt in the area. The 'middle uplift' zone in the orogenic belt is often dominated by metamorphic iron ore controlled by stratigraphy within the Proterozoic strata, and the late Paleozoic and Mesozoic marine volcanic rock iron ore combinations are dominant within the island arc zone. Karnian and hydrothermal iron deposits are distributed. Iron deposits are often concentrated in volcanic basins, volcanoes, and sub-volcanic structures; and back-arc basins form deposited iron deposits. Orogen
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