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  • Print publication year: 2012
  • Online publication date: November 2012

Chapter 14 - Metamorphic rocks

Summary

Metamorphism is the sum of all changes that take place in a rock when it experiences changes in temperature, pressure (both lithostatic and directed), or composition of fluids in the environment. The important word in this definition is change. The changes may be physical, chemical, isotopic, or any combination of these. The original rock, known as the protolith, can be igneous, sedimentary, or a previous metamorphic rock. Most metamorphic reactions are very slow, so time is important in determining how complete a change may be. Some rocks are more reactive than others, and higher temperatures and the presence of fluids also speed up reactions. Changes that take place while rocks are heating are referred to as prograde and those occurring during cooling are referred to as retrograde. Changes that take place at low temperatures during the compaction and lithification of sediments could, in the broadest sense, be considered metamorphic, but normally only reactions taking place above about 150°C are dealt with in metamorphic studies, but the division is arbitrary. Reactions have a greater chance of going to completion at the higher temperatures experienced by metamorphic rocks than they do in sedimentary rocks. At the highest temperatures, metamorphic rocks begin to melt, producing mixtures of metamorphic and igneous rocks known as migmatites.

FURTHER READING
Barrow, G. 1983 On an intrusion of muscovite-biotite gneiss in the southeast Highlands of Scotland, and its accompanying metamorphismQuarterly Journal of the Geological Society of London 49 330
Bowen, N. L. 1940 Progressive metamorphism of siliceous limestone and dolomiteJournal of Geology 48 225
Eskola, P. 1920 The mineral facies of rocksNorsk Geologisk Tidsskrift 6 143
Philpotts, A. R.Ague, J. J. 2009 Principles of Igneous and Metamorphic PetrologyCambridge University PressCambridge
Spear, F. S.Cheney, , J. T. 1989 A petrogenetic grid for pelitic schists in the system SiO2-Al2O3-FeO-MgO-K2O-H2OContributions to Mineralogy and Petrology 101 149
Thompson, J. B. 1957 The graphical analysis of mineral assemblages in pelitic schistsAmerican Mineralogist 42 842
Vernon, R. H.Clarke, G. L. 2008 Principles of Metamorphic PetrologyCambridge University PressCambridge
Yardley, B. W. D.MacKenzie, W. S.Guilford, C. 1990 Atlas of Metamorphic Rocks and Their TexturesLongmanHarlow, U.K