Metamorphism of Pelites

Winkler, Helmut G. F.

doi:10.1007/978-1-4612-9828-1_14

Metamorphism of Pelites

Helmut G. F. Winkler³

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Abstract

Slates, phyllites, and mica schists are derived from clay. They belong to the large group of metamorphic rocks known as metapelites. In addition to quartz, the following minerals are common constituent of these rocks:

Pyrophyllite, andalusite, kyanite, sillimanite
Staurolite
Chloritoid, cordierite
Chlorite, almandine-rich garnet
The K-bearing micas phengite, muscovite, and biotite
The Na-bearing mica paragonite and solid solutions of paragonite and phengite/muscovite
The Ca-bearing mica margarite
Stilpnomelane
Alkali feldspar is present in some very-low and low-grade rocks and is widespread in high-grade rocks where it commonly takes the place of muscovite.

Most of there minerals may be gaphically presented in an AFM diagram; see Figure 5–10 in Chapter 5.

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Authors and Affiliations

Institute of Mineralogy and Petrology, University of Göttingen, Germany
Helmut G. F. Winkler (Professor and Director)

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Helmut G. F. Winkler
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Geological Survey, Ottawa, Canada
Edgar Froese

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Winkler, H.G.F. (1974). Metamorphism of Pelites. In: Froese, E. (eds) Petrogenesis of Metamorphic Rocks. Springer, New York, NY. https://doi.org/10.1007/978-1-4612-9828-1_14

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DOI: https://doi.org/10.1007/978-1-4612-9828-1_14
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