Metamorphic Minerals, Processes, and Structures

Tyrrell, G. W.

doi:10.1007/978-94-011-6026-1_16

G. W. Tyrrell A.R.C.Sc., F.G.S., F.R.S.E., D.Sc.²

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Abstract

The mineral transformations which take place in metamorphism depend, in the first instance, on the composition of the original rock, and then on the kind of metamorphism to which it has been subjected.

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References

Holmes, Petrographic Methods and Calculations, 1921, pp. 372–83; L. Milch, op. cit. supra, pp. 310–15; Grubenmann and Niggli, op. cit. supra, pp. 413–77; Becke, op. cit. supra.
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Authors and Affiliations

University of Glasgow, Glasgow, UK
G. W. Tyrrell A.R.C.Sc., F.G.S., F.R.S.E., D.Sc. (Lecturer in Geology)

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G. W. Tyrrell A.R.C.Sc., F.G.S., F.R.S.E., D.Sc.
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Tyrrell, G.W. (1978). Metamorphic Minerals, Processes, and Structures. In: The Principles of PETROLOGY. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-6026-1_16

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DOI: https://doi.org/10.1007/978-94-011-6026-1_16
Publisher Name: Springer, Dordrecht
Print ISBN: 978-0-412-21500-1
Online ISBN: 978-94-011-6026-1
eBook Packages: Springer Book Archive

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