Water-fluxed crustal melting produces Cordilleran batholiths

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Water-fluxed crustal melting produces Cordilleran batholiths

Most granites and related calc-alkaline silicic volcanic rocks from the United States and New Zealand Cordillera are saturated with zircon between 65 and 70 wt% SiO2. For this silica interval, zircon saturation temperatures (Tzr) are universally lower (<800 °C) than those expected by dehydrat...

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Bibliographic Details
Main Authors:	Collins, Bill, Huang, H., Jiang, X.
Format:	Journal Article
Published:	Geological Society of America 2016
Online Access:	http://hdl.handle.net/20.500.11937/54789

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