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Experimental and thermal constraints on the deep-seated parentage of some granitoid magmas in subduction zones

Wyllie, P. J. (1983) Experimental and thermal constraints on the deep-seated parentage of some granitoid magmas in subduction zones. In: Migmatites, Melting and Metamorphism: Proceedings of the Geochemical Group of the Mineralogical Society. Shiva , Nantwich, pp. 37-51. ISBN 0906812267. https://resolver.caltech.edu/CaltechAUTHORS:20160219-080023614

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Abstract

Regional metamorphism, migmatites and granites certainly owe their origin to influx of heat from the mantle. There is evidence that heat may be accompanied by material. This review is concerned with the deep source rocks, the fluid products, and the processes which contribute to the addition of material from the mantle into the crust, specifically at convergent plate boundaries where regional metamorphism and magmatic processes reach their most spectacular development in the formation of batholiths, calderas, andesites and rhyolite ash eruptions.


Item Type:Book Section
Additional Information:© 1983 Shiva Publishing Limited. I thank all of my colleagues who helped gather the data that made this review possible and National Science Foundation for grant EAR 8108626.
Funders:
Funding AgencyGrant Number
NSFEAR 8108626
Record Number:CaltechAUTHORS:20160219-080023614
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20160219-080023614
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:64600
Collection:CaltechAUTHORS
Deposited By: Tony Diaz
Deposited On:19 Feb 2016 19:11
Last Modified:03 Oct 2019 09:39

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