Enstatite is a mineral; the magnesium endmember of the pyroxene silicate mineral series enstatite (MgSiO 3) – ferrosilite (FeSiO 3). The magnesium rich members of the solid solution series are common rock-forming minerals found in igneous and metamorphic rocks.

Enstatite: Carlson W D, Swinnea J S, Miser D E (1988) Stability of orthoenstatite at high temperature and low pressure American Mineralogist 73 1255-1263: 1988: 0: 293: 0001244: Enstatite: Angel R J, Gasparik T, Finger L W (1989) Crystal structure of a Cr-bearing pyroxene American Mineralogist 74 599-603: 1989: 0: 293: 0001644: Enstatite

Jul 1, 2024 · Enstatite is a mineral that belongs to the pyroxene group, which is a class of silicate minerals. It is known for its unique crystalline structure and a range of physical properties that make it an interesting and important mineral in various scientific fields.

enstatite, common silicate mineral in the pyroxene family. It is the stable form of magnesium silicate (MgSiO 3, often with up to 10 percent iron) at low temperatures. See orthopyroxene. A micrograph of an enstatite crystal taken from an ultramatic rock.

Detailed description, properties, locality information guide about the pyroxene mineral enstatite and hypersthene.

Apr 22, 2023 · As a mineral, enstatite is fairly common, but gem-quality enstatite specimens are rare and exotic finds. Ready to learn more? In this guide, we’ll cover all of enstatite’s properties, varieties, prices, meanings, and more!

Enstatite (MgSiO 3) is the magnesium endmember of the pyroxene mineral group. This mineral consists of chains of linked silica tetrahedra with magnesiums that are coordinated by two opposing silicate chains.

Enstatite. Comments: Single, terminated, brown, transparent to translucent enstatite crystal. Location: Mpwa-Mpwa, Tanzania. Scale: 17x17x27 mm. © Dan Weinrich

Enstatite is a relatively common mineral and is found in metamorphic and some igneous rocks as well as in stony and iron meteorites. It forms a solid solution series with the minerals hypersthene and ferrosilite.

Enstatite crystals growing in an epitaxial relationship to a host Ilmenite crystal. It looks as though the ilmenite pierces through and splits a single enstatite crystal. But the ilmenite forms the substrate for the epitaxial growth of the two parallel enstatite crystals.