AOlivine
BAmphibole
CPyroxene
DMica
Answer:
C. Pyroxene
Read Explanation:
Pyroxene Group Minerals
Pyroxenes are a group of inosilicate minerals forming an important component of igneous and metamorphic rocks. They are characterized by their chemical formula which generally involves chains of SiO4 tetrahedra linked by ions such as iron (Fe), magnesium (Mg), calcium (Ca), and aluminum (Al).
Key Characteristics and Significance
Abundance in Earth's Crust: Pyroxenes constitute approximately 10% of the Earth's crust by weight, making them one of the most abundant mineral groups. They are particularly prevalent in mafic and ultramafic igneous rocks like basalt and gabbro, which form a significant part of the oceanic crust and continental volcanic regions.
Presence in Meteorites: Pyroxenes are also found in meteorites, including stony meteorites (chondrites and achondrites), which provides insights into the composition of the early solar system and extraterrestrial materials. This extraterrestrial presence is a unique characteristic that distinguishes them from some other common crustal minerals.
Geological Formation: They are typically formed under high temperatures and pressures, often found in mantle-derived magmas and deep crustal environments.
Structural Feature: Their crystal structure features single chains of linked SiO4 tetrahedra, which gives them their characteristic prismatic cleavage angle of around 87° and 93°.
Types of Pyroxenes: Common examples include enstatite (MgSiO3), ferrosilite (FeSiO3), and diopside (CaMgSi2O6). The solid solution series between these end-members leads to a wide variety of pyroxene compositions.
