| Kanoite | |
| Category: | Silicate mineral (pyroxene, inosilicate) |
| Imasymbol: | Knt[1] |
| Molweight: | 246.73 g/mol |
| System: | Monoclinic |
| Class: | Prismatic (2/m) (same H-M symbol) |
| Symmetry: | P21/c |
| Unit Cell: | a = 9.73, b = 8.93 c = 5.26 [Å]; β = 108.56°; Z = 4 |
| Color: | Light pinkish brown |
| Twinning: | Polysynthetic |
| Cleavage: | Perfect on, - = 88° |
| Mohs: | 6 |
| Luster: | vitreous |
| Refractive: | nα = 1.715 nβ = 1.715 nγ = 1.728 |
| Opticalprop: | Biaxial (+) |
| 2V: | 40-42 measured |
| Birefringence: | 0.0130 |
| Gravity: | 3.66 |
| Diaphaneity: | Semitransparent |
| References: | [2] [3] |
Kanoite is a light pinkish brown silicate mineral that is found in metamorphic rocks. It is an inosilicate and has a chemical formula of .[4] It is a member of pyroxene group and clinopyroxene subgroup.[5]
Kanoite crystallizes in the monoclinic crystal system. Its Hermann–Mauguin Symbol is 2/m. Under this crystal system, the three axes of the crystal are all different in length. The a and the b axes are perpendicular, and b and c axes are perpendicular. The a and c axes make an oblique shape. The axial ratio for kanoite is a:b:c =1.0894:1:0.5884 and the cell dimensions are: a = 9.73, b = 8.93 and c = 5.26 Å with Z = 4.[2] Kanoite has a 2-fold axis and a mirror plane.
Kanoite is birefringent. It occurs as a mineral has 3 different indices of refraction. When the light passes through the Kanoite medium, the light splits due to unequal reflection from the crystal faces. As kanoite is birefringent, it is also anisotropic. In an anisotropic mineral, the velocity of light differs as the direction of the crystal changes.
Kanoite is a rare mineral which was found in Tatehira mine, Kumaishi, Oshima Peninsula, Hokkaido, Japan in 1977. In the type locality kanoite occurs along a joint that cuts a pyroxmangite-cummingtonite metamorphic rock in a manganese ore deposit. The region has undergone contact metamorphism as magma intruded the area. It was named to honor Hiroshi Kano, a petrology professor at Akita University in Japan.[4]
It has also been reported from Broken Hill, New South Wales, Australia, the Semail Ophiolite in Oman, and the Balmat–Edwards zinc district, Saint Lawrence County, New York.[2]