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Geological Society, London, Special Publications; 1998; v. 138; p. NP;
DOI: 10.1144/GSL.SP.1996.138.01.16
© 1998 Geological Society of London

About this title

Although it has long been recognized that what ultimately drives metamorphism and metamorphic reactions is heat, what was less certain is the distribution of heat within the crust, the type and location of major heat sources and the rates of heat flux through crustal rocks. This book explores the factors that control metamorphism and rates of metamorphic processes.

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This 250-word extract was created in the absence of an abstract.