Abstract
The rock name eclogite was coined by HaĆ¼y, a founder of crystallography, in 1822. Since the original definition of the name was vague, its meaning was gradually settled through its usage in later years. According to the generally established usage in the first half of the twentieth century, it means a rock mainly composed of omphacite and almandine-pyrope-grossular garnet. Omphacite is a clinopyroxene containing diopside, hedenbergite and jadeite components, and quite frequently some acmite. However, no rigid limitations were given for the composition ranges of these minerals. Thus, some authors called diopside-almandine rocks eclogite. Small amounts of quartz, kyanite, olivine, orthopyroxene, amphibole and rutile may be present, but not plagioclase.
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Ā© 1965 Akiho Miyashiro
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Miyashiro, A. (1965). Eclogites and the Eclogite Facies. In: Metamorphism and Metamorphic Belts. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-6836-6_15
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DOI: https://doi.org/10.1007/978-94-011-6836-6_15
Publisher Name: Springer, Dordrecht
Print ISBN: 978-0-04-550026-0
Online ISBN: 978-94-011-6836-6
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