Disequilibrium metamorphism of stressed lithosphere

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Disequilibrium metamorphism of stressed lithosphere

© 2015 Elsevier B.V. Most changes in mineralogy, density, and rheology of the Earth's lithosphere take place by metamorphism, whereby rocks evolve through interactions between minerals and fluids. These changes are coupled with geodynamic processes and have first order effects on the global geo...

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Bibliographic Details
Main Authors:	Jamtveit, B., Austrheim, H., Putnis, Andrew
Format:	Journal Article
Published:	Elvevier 2016
Online Access:	http://hdl.handle.net/20.500.11937/9885

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