Formation of low-δ18O magmas of the Kangerlussuaq Intrusion by addition of water derived from dehydration of foundered basaltic roof rocks
Author:
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
http://link.springer.com/content/pdf/10.1007/s00410-015-1134-7.pdf
Reference86 articles.
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2. Beard JS, Lofgren GE (1991) Dehydration melting and water-saturated melting of basaltic and andesitic greenstones and amphibolites at 1, 3, and 6.9 kb. J Petrol 32:365–401
3. Bindeman I (2008) Oxygen isotopes in mantle and crustal magmas as revealed by single crystal analysis. Rev Mineral Geochem 69(1):445–478
4. Bindeman IN, Valley JW (2001) Low-δ18O rhyolites from Yellowstone: magmatic evolution based on analyses of zircon and individual phenocrysts. J Petrol 42:1491–1517
5. Bindeman IN, Valley JW (2003) Rapid generation of both high- and low-δ18O, large volume silicic magmas at Timber Mountain/Oasis Valley caldera complex, Nevada. Geol Soc Am Bull 115(5):581–595
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