high intensity magnetic separator

Mineral composition and intercalation of the ore: it is a sedimentary metamorphic rock, the shallow layer is dominated by red iron quartzite, and the deep layer is transitive to magnetite quartzite. The mineral composition of the ore is relatively simple, mainly magnetite, hematite, hematite; Gangue minerals are dominated by quartz, followed by actinite, amphibole minerals, apatite inclusions and a small amount of common amphibole and pyroxene. Trace minerals include apatite, pyrite, chalcopyrite, and later altered chlorite, carbonate, biotite and other minerals. The ore samples taken in this test are shallow lean hematite. PTMS magnetic separator can remove the iron (FE2O3) inside.

PTMS magnetic separation

The ore structure is mainly banded, accompanied by crumpled structure. The structure of the ore is dominated by granular metasomatism and metasomatism. The magnetite in the iron ore strip has a semiidiomorphic and self-deformable crystal structure with uneven particle size, while the magnetite inclusions in the quartz have a fine self-crystalline structure. PTMS magnetic separator can remove the iron (FE2O3) inside.

what is magnetic separation in Quartz?

Oxidative metasomatism occurs around the magnetite and in cleavage fractures, resulting in marginal metasomatism, network and residual structures. The average particle size of iron minerals and gangue minerals is 62.79 and 80.25 respectively. PTMS magnetic separator can remove the iron (FE2O3) inside.
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