Raw Mineral Separation

During the Permian Period of the Paleozoic Era, approximately 290 million years ago, the indo-china movement was highly active, marking a significant geological period in China's geological history. During this time, three-quarters of China's current landmass completed its assembly and unification. In the region now known as Huade County, Ulanqab, Inner Mongolia Plateau (with coordinates ranging from East Longitude: 113°56'45" to 113°57'23" and North Latitude: 41°52'36" to 41°52'56"), extensive geological changes occurred. The original coarse-grained pegmatitic structure, primarily composed of pegmatite silicate,  was significantly affected by the Late Triassic Yanshan tectonic period (about 250 million years ago), leading to the formation of three distinct translational fault zones. The mineral bodies and magma erupted along these fault zones, and a complex and unique rock foundation gradually formed, covering an overall area of 16.8 square kilometers. The three translational fault structures in different directions created a core enrichment area, infusing various trace elements, including rare earth elements, into the mineralized coarsegrained pegmatitic rocks and magma. This process led to the formation of large phenocrystalline feldspar, tea -colored quartz, and biotite, among other minerals. Under the influence of strong internal stress and geological structural conditions, a secondary mineralization occurred as a result of the subsequent magma intrusion. These transitional intermediate products, enriched with rare earth elements and light metal oxides, underwent further fusion and interaction with the magma, causing the mineral components to fractionate again. During the alternating crystallization of minerals, elements such as the lanthanide series, light metals, selenium, and nutrients required by plants were melted or crystallized into different material forms of the ore body, resulting in the formation of a unique new mineral species known as "wulan crystal".