Formation of low-δ18O rhyolites after caldera collapse at Yellowstone, Wyoming, USA
Author:
Publisher
Geological Society of America
Subject
Geology
Reference24 articles.
1. Direct evidence for the origin of low-18O silicic magmas: quenched samples of a magma chamber's partially-fused granitoid walls, Crater Lake, Oregon
2. Low-18O silicic magmas: why are they so rare?
3. SHRIMP U-Pb dating of the preeruption growth history of zircons from the 340 ka Whakamaru Ignimbrite, New Zealand: Evidence for >250 k.y. magma residence times
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