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Granitic Rocks

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Part of the Minerals, Rocks and Inorganic Materials book series (MINERALS,volume 5)

Abstract

Granites are coarse-grained crystalline rocks of igneous aspect composed of quartz, feldspar, and micas or ferromagnesian minerals such as hornblende. In this chapter we shall include under the heading of granitic rocks such related varieties as quartz monzonite, granodiorite, quartz diorite, and monzonite — all of which are mineralogically similar to granites. These granitic rocks collectively make up the large batholiths of the world, and many of the smaller stocks, laccoliths, dikes, and sills. They are by far the most abundant plutonic igneous rocks in the continental crust. If the scope of the definition were widened to encompass gneissic rocks of similar mineral composition, which may have had granites as parents, many of the rocks of the Precambrian Shield areas would also be included.

Keywords

  • Partial Melting
  • Continental Crust
  • Granitic Rock
  • Parent Magma
  • Initial Ratio

These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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© 1972 Springer-Verlag Berlin, Heidelberg

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Faure, G., Powell, J.L. (1972). Granitic Rocks. In: Strontium Isotope Geology. Minerals, Rocks and Inorganic Materials, vol 5. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-65367-4_5

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  • DOI: https://doi.org/10.1007/978-3-642-65367-4_5

  • Publisher Name: Springer, Berlin, Heidelberg

  • Print ISBN: 978-3-642-65369-8

  • Online ISBN: 978-3-642-65367-4

  • eBook Packages: Springer Book Archive