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Metamorphism of Ultramafic Rocks: Systems MgO-SiO2-CO2-H2O and MgO-CaO-SiO2-H2O

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Abstract

Two different rock types are predominantly composed of MgO and SiO2: ultramafic rocks and the much rarer siliceous magnesite rocks. The major mineral constituents of ultramafic rocks are olivine, orthopyroxene, and/or clinopyroxene, and the MgO/FeO ratio of the rocks is very high. CaO is another component present in clinopyroxene.

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© 1979 Springer Science+Business Media New York

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Winkler, H.G.F. (1979). Metamorphism of Ultramafic Rocks: Systems MgO-SiO2-CO2-H2O and MgO-CaO-SiO2-H2O. In: Petrogenesis of Metamorphic Rocks. Springer Study Edition. Springer, New York, NY. https://doi.org/10.1007/978-1-4757-4215-2_11

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  • DOI: https://doi.org/10.1007/978-1-4757-4215-2_11

  • Publisher Name: Springer, New York, NY

  • Print ISBN: 978-0-387-90413-9

  • Online ISBN: 978-1-4757-4215-2

  • eBook Packages: Springer Book Archive

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