Inosilicates: Pyroxenes Flashcards
Inosilicates
A group of minerals whose defining characteristic is their chain arrangement of silica (SiO4) tetrahedra.
Single Chain Inosilicates
Pyroxenes
Double chain Inosilicates
Amphiboles
Pyroxenes General Formula
X Y Si2 O6
2 main solid solution minerals
Augite (Au) - Diopside (Di) CaMg, Hedenbergite (He) CaFe
Hypersthene (Hy) - Enstatite (En) Mg2, Ferrosilite (Fs) Fe2
Augite (Au)
Solid solution of:
Diopside (Di) CaMg
Hedenbergite (He) CaFe
A common Clinopyroxene
Hypersthene (Hy)
Solid solution of:
Enstatite (En) Mg2,
Ferrosilite (Fs) Fe2
A common Orthopyroxene
Enstatite (En)
Magnesium Pyroxene
Mg2 Si2 O6
Ferrosilite (Fs)
Iron Pyroxene
Fe2 Si2 O6
Diopside (Di)
Calcium Magnesium Pyroxene
Ca Mg Si2 O6
Hedenbergite (He)
Calcium Iron Pyroxene
Ca Fe Si2 O6
3 rare pyroxenes
Aegirine - Na Fe Si2 O6
Jadite - Na Al Si2 O6
Omphacite
Aegirine
Na Fe Si2 O6
Jadeite
Na Al Si2 O6
Structure of Pyroxenes
Pyroxenes are formed by series of SiO4 tetrahedra sharing a common oxygen on two corners forming a single chain parallel to the c-axis. These chains are liked laterally with octahedron layers (100 plane) which contain the cation
Orthopyroxene minerals composition
Orthopyroxenes contain a solid solution of En-Fs
Enstatite-Ferrosilite
Hypersphene is the most common orthopyroxene mineral formed
Clinopyroxenes mineral composition
Contain Calcium
Diopsite + Hedenbergite With some En-Fs
Exsolution
process through which an initially homogeneous solid solution separates into at least two different crystalline minerals without the addition or removal of any materials. In most cases, it occurs upon cooling below the temperature of mutual solubility or stability of the solution.
Miscibility
Miscibility is the property of two substances to mix in all proportions, forming a homogeneous mixture.
Orthopyroxene Crystal System
Orthorhombic
Clinopyroxene crystal system
Monoclinic
Orthopyroxene colour in thin sections
Pale, subtle pinkish to greenish pleochroism in some
Clinopyroxene colour in thin sections
Colourless or grey/pale green/pale brown: darker if Fe rich
Pyroxene form in thin sections
Subhedral stubby prisms, basal sections 4-8 sided