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Magnetite-apatite Ore Deposits Can Be Classified Into Two Major Groups:
Get Magnetite-apatite Ore Deposits Can Be Classified Into Two Major Groups:
; and b) low-Ti, magnetite deposits with variable amounts of apatite (Kiruna type ores) principally associated with volcanic rocks. The origin of the first type is generally accepted to be magmatic, with liquid immiscibility between silicate magma and iron-titanium-phosphorous-oxide magma, small percent partial melting of Fe and P-rich crustal rocks, or extreme crystal fractionation the most commonly cited processes (Philpotts, 1967; Kolker, 1982; Barton & Johnson, 1996; Naslund, et al., 2000).
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Mineralization FAQ
Apatite is widely distributed in all classes of rock –igneous, sedimentary and metamorphic. Large, well-formed crystals are, for the most part, limited to metamorphic rocks.
Apatite is widely distributed in all rock types ( igneous, sedimentary and metamorphic), but usually as small disseminated grains, or cryptocrystalline fragments. Large, well-formed crystals can be found in certain contact metamorphic rocks.
Nearly all the earth's iron comes from ore deposits in rocks formed more than 1.8 billion years ago. These began forming when the first organisms capable of photosynthesis began releasing oxygen into the world's oceans, which combined with dissolved iron to produce haematite or magnetite.
Iron ore occurs most abundantly in the form of oxides. Other forms are carbonates, hydroxides, sulphides and silicates. It is also found in association with titanium dioxide. Commercially, the most important minerals of iron are in the form of oxides, i.e., hematite (Fe₂O₁) and magnetite (Fe3O4).
Apatite is found in igneous, metamorphic and sedimentary rocks. Apatite is not one mineral but rather a group of phosphate minerals.
Iron ores are rocks from which metallic iron can be economically extracted. Most deposits of iron ore in the world are found in rocks known as banded iron formations (BIFs). These are sedimentary rocks that have alternating layers of iron-rich minerals and a fine-grained silica rock called chert.
Apatite is a phosphate mineral that has a hardness of 5 on the Mohs scale, making it too soft to be widely used as a gemstone for jewelry. Apatites are transparent to translucent, most commonly green to blue, but can also be colorless, yellow, violet, pink or brown.
Apatite is a very common early-formed accessory mineral in nearly all type of igneous rocks. Apatite is also concentrated by late magmatic segregation, and it appears in granite pegmatite.
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