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.
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
Preview
Unable to display preview. Download preview PDF.
Author information
Authors and Affiliations
Rights and permissions
Copyright information
© 1972 Springer-Verlag Berlin, Heidelberg
About this chapter
Cite this chapter
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
Download citation
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