Epidote - Ca2(Fe,Al)3(SiO4)3(OH)
Named in 1801 by Rene Just Hauy from the Greek "Epidosis" = "increase" because the base of the rhombohedral prism has one side larger than the other.The Epidote structure consists of octahedral AlO6 groups sharing edges to form continuous chain parallel to b axis. In one-third of the octahedral groups, Al3+ is surrounded by four O2- and two (OH)-. The octahedral chains are linked by silicon, in SiO4 and SiO7 groups, sharing oxygen ions with aluminum. Larger Ca2+ ions fill interchain voids to produce electrostatic neutrality. The resulting basic composition is Ca2Al3O(SiO4)(SiO7)OH and the structure is dimorphous, as orthorhombic and monoclinic forms. Significant Al3+ may be replaced by Fe3+, Mn3+, or even Cr3+, and Ca2+ may be partly replaced by Ce3+, La3+, Y3+ and other rare earth elements with equal replacement of Fe3+ and Al3+ by Fe2+ to maintain electrostatic balance.
Orthorhombic varieties:
♦ Zoisite Ca2Al3O(SiO4)(SiO7)OH
♦ Thulite Ca2(Al,Fe3+, Mn3+)3O(SiO4)(SiO7)OH
Monoclinic varieties:
♦ Clinozoisite Ca2Al3O(SiO4)(SiO7)OH
♦ Pistacite Ca2Fe3+Al2O(SiO4)(SiO7)OH
♦ PiemontiteCa2(Al,Fe3+,Mn3+)3O(SiO4)(SiO7)OH
♦ Allanite (Ca,Ce,La)2(Al,Fe3+,Fe2+)3O(SiO4)(SiO7)OHOH
♦ Tawmawite Ca2(Al,Fe3+,Cr3+)3O(SiO4)(SiO7)OH
♦ Hancockite (Ca,Pb,Sr)2(Al,Fe3+)3O(SiO4)(SiO7)OH
The common epidote minerals are formed largely under conditions of low to medium grade metamorphism in association with Ca-poor plagioclase. At higher grades, epidote combines with albite to form Ca-rich plagioclase.
Optical properties:
Color: pale yellow, pale green
Form: fine to coarse aggregate are common
Cleavage: basal cleavage (001) perfect
Interference colors: mild to strong birefringence. the colors often vary within the same crystal (harlequin colors)
Relief: high
Bibliography
• Cox et al. (1979): The Interpretation of Igneous Rocks, George Allen and Unwin, London.
• Howie, R. A., Zussman, J., & Deer, W. (1992). An introduction to the rock-forming minerals (p. 696). Longman.
• Le Maitre, R. W., Streckeisen, A., Zanettin, B., Le Bas, M. J., Bonin, B., Bateman, P., & Lameyre, J. (2002). Igneous rocks. A classification and glossary of terms, 2. Cambridge University Press.
• Middlemost, E. A. (1986). Magmas and magmatic rocks: an introduction to igneous petrology.
• Shelley, D. (1993). Igneous and metamorphic rocks under the microscope: classification, textures, microstructures and mineral preferred-orientations.
• Vernon, R. H. & Clarke, G. L. (2008): Principles of Metamorphic Petrology. Cambridge University Press.
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