Search results
Orthopyroxenes are a group of minerals ranging from pure MgSiO3 (enstatite) to pure FeSiO3 (ferrosilite). Bronzite and hypersthene are orthopyroxenes mid-way between these two end members. As the particular orthopyroxene mineral described is not always identified, all reported orthopyroxene occurrences are grouped together. Orthopyroxenes are relatively widespread as a primary mineral in ...
Пироксени. Пироксени су група силикатних минерала, која припада поткласи иносиликата. Минерали из ове групе су значајни петрогени минерали, који улазе у састав многих врста стена ...
Harzburgite, an ultramafic, igneous rock, is a variety of peridotite consisting mostly of the two minerals olivine and low- calcium (Ca) pyroxene ( enstatite ); it is named for occurrences in the Harz Mountains of Germany. It commonly contains a few percent chromium -rich spinel as an accessory mineral. Garnet -bearing harzburgite is much less ...
Clinopyroxene thermobarometry is a scientific method that uses the mineral clinopyroxene to determine the temperature and pressure of the magma when the mineral crystalized. Clinopyroxene is found in many igneous rocks, so the method can be used to determine information about the entire rock. Many different minerals can be used for ...
Download reference work entry PDF. The orthopyroxenes are an important series of rock-forming minerals. They are the orthorhombic members of the pyroxene group of silicates and consist essentially of a simple chemical series of (Mg,Fe)SiO 3 minerals, in contrast with the larger subgroup of monoclinic pyroxenes ( clinopyroxenes , q.v.) which ...
The English Wikipedia is the primary [a] English-language edition of Wikipedia, an online encyclopedia. It was created by Jimmy Wales and Larry Sanger on 15 January 2001, as Wikipedia's first edition. English Wikipedia is hosted alongside other language editions by the Wikimedia Foundation, an American nonprofit organization.
Anorthosite ( / əˈnɔːrθəsaɪt /) is a phaneritic, intrusive igneous rock characterized by its composition: mostly plagioclase feldspar (90–100%), with a minimal mafic component (0–10%). Pyroxene, ilmenite, magnetite, and olivine are the mafic minerals most commonly present. Anorthosites are of enormous geologic interest, because it is ...
