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This title is printed to order. This book may have been self-published. If so, we cannot guarantee the quality of the content. In the main most books will have gone through the editing process however some may not. We therefore suggest that you be aware of this before ordering this book. If in doubt check either the author or publisher’s details as we are unable to accept any returns unless they are faulty. Please contact us if you have any questions.
This work covers the subject of the petrology of the metamorphic rocks, including such subjects as rock and mineral compositions and their relationship, metamorphism associated with igneous intrusions, dynamic metamorphism, extra-terrestrial metamorphism and metamorphism in collision zones. The book uses examples of the field relationships of metamorphic rocks and their appearance in thin section; discusses the thermodynamic and analytic methods concerned; describes methods for determining the temperatures and deformations of the rocks and demonstrates how thermodynamic modelling enables them to be interpreted as the outcome of plate tectonics.
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This title is printed to order. This book may have been self-published. If so, we cannot guarantee the quality of the content. In the main most books will have gone through the editing process however some may not. We therefore suggest that you be aware of this before ordering this book. If in doubt check either the author or publisher’s details as we are unable to accept any returns unless they are faulty. Please contact us if you have any questions.
This work covers the subject of the petrology of the metamorphic rocks, including such subjects as rock and mineral compositions and their relationship, metamorphism associated with igneous intrusions, dynamic metamorphism, extra-terrestrial metamorphism and metamorphism in collision zones. The book uses examples of the field relationships of metamorphic rocks and their appearance in thin section; discusses the thermodynamic and analytic methods concerned; describes methods for determining the temperatures and deformations of the rocks and demonstrates how thermodynamic modelling enables them to be interpreted as the outcome of plate tectonics.