Structural linkage among double-chain silicates
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The defining characteristic of the structures of all amphiboles (double-chain silicates) is that they consist of (Si,Al) tetrahedra linked together to form chains which are twice as wide as those found in pyroxenes. The apical oxygens of the tetrahedra in these chains are situated below and above a ribbon of MO6 octahedra. For further information on the structural linkage among silicate minerals, please visit https://skfb.ly/6SBZu or https://skfb.ly/6Rt9V. Note that the color code used in these models is CPK. Visit http://geology.uaic.ro/muzee/mineralogie for more information. Concept and 3D modeling by dr. Andrei Ionut APOPEI.
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