Ilmenite
A species of Ilmenite Group, Also known as Axotomous Eisenerz, Haplotypite, Mänaken, Para-Ilmenite, Titanic Iron Scientific name : Ilmenite Mineral Group : Ilmenite Group
Ilmenite, A species of Ilmenite Group
Also known as:
Axotomous Eisenerz, Haplotypite, Mänaken, Para-Ilmenite, Titanic Iron
Scientific name: Ilmenite
Mineral Group: Ilmenite Group
Content
Description People often ask General Info
Description
Commonly found across the globe, ilmenite has also been found in moon rocks! It is used for its titanium content, processed into ultra-strong metal alloys. It is also mined to create titanium dioxide, which is useful for coloration and polishing. When eroded by nature, it forms beautiful black sand beaches which indicate a prominent veins is close by.
Physical Properties
Colors
Iron black, black
Luster
MetallicSubMetallic
Diaphaneity
Opaque
Chemical Properties
Chemical Classification
Oxides
Formula
Fe2+TiO3
Elements listed
Fe, O, Ti
Common Impurities
Mn, Mg, V
People often ask
General Info
Usage
Ilmenite is an important ore of titanium, which is used to make things like tools, bicycle frames, artificial human joints, and high performance parts. Ilmenite is also used to make titanium dioxide, which is a white, reflective material. It is typically used as a pigment for anything from paper to toothpaste, after the mineral is ground into a powder and impurities are removed.
Composition
Ilmenite crystallizes in the trigonal system. The ilmenite crystal structure consists of an ordered derivative of the corundum structure; in corundum all cations are identical but in ilmenite Fe and Ti ions occupy alternating layers perpendicular to the trigonal c axis. Containing high spin ferrous centers, ilmenite is paramagnetic. Ilmenite is commonly recognized in altered igneous rocks by the presence of a white alteration product, the pseudo-mineral leucoxene. Often ilmenites are rimmed with leucoxene, which allows ilmenite to be distinguished from magnetite and other iron-titanium oxides. The example shown in the image at right is typical of leucoxene-rimmed ilmenite. In reflected light it may be distinguished from magnetite by more pronounced reflection pleochroism and a brown-pink tinge. Samples of ilmenite exhibit a weak response to a hand magnet.