This dataset describes an iron ore deposit in Tibet, with the following information:
The ore type is classified according to the natural assemblage characteristics of minerals in the ore and the characteristics of the ore-bearing rock series. Within the mining area, the iron ore is entirely of the hornblende schist type. Based on the content characteristics of valuable components in the ore, two ore types can be further distinguished:
1. Dense massive magnetite (high-grade ore): Found in the central part of the ore layer, appearing as black to gray-black dense massive ore with conchoidal fractures. It exhibits euhedral to subhedral granular texture, and has dense massive and densely disseminated structures. The ore is mainly composed of magnetite, which occurs as medium to coarse-grained, euhedral to subhedral crystals, uniformly and densely distributed. Gangue minerals are primarily hornblende and biotite, followed by minor amounts of calcite, epidote, dolomite, etc. Banded magnetite (low-grade ore): occurs near the top and bottom of the ore layer or interbedded within high-grade ore layers, exhibiting a scaly recrystallized texture and banded structure. It consists of magnetite and minor siliceous material. The ore is stained brownish-red by limonite, and in hand specimens, pyrrhotite crystals are observed, with hematite and limonite impregnating along cleavages and fractures. Iron mainly occurs in magnetite, accounting for 85. 23 percent, followed by occurrence in limonite (7.1%), and minor amounts in silicate iron, carbonate iron, and sulfide minerals. Associated beneficial components in the iron ore include manganese, with variable content ranging from 0.05% to 2.97% and an average of 1.86%, which currently has no economic value. (3) Harmful components—Sulfur: The sulfur content in the iron ore varies within a narrow range of 0.060% to 0.087%, averaging 0.076%. Sulfur mainly occurs in the form of iron sulfides such as pyrite, pyrrhotite, and marcasite, classifying this as low-sulfur ore. Phosphorus: The phosphorus content in the ore is also low, at 0.0230. between 0.042%, averaging 0.035%, mainly occurring in apatite minerals, belonging to low-grade phosphate ore.