Storage, Ascent, and Release of Silicic Magma in Caldera-Forming Eruptions
The mechanisms and timescales associated with the triggering of caldera-forming eruptions remain ambiguous and poorly constrained. Do such eruptions start vigorously, then escalate, or can there be episodicity? Are they triggered through internal processes (e.g. recharge, buoyancy), or can external...
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Language: | en_US |
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University of Oregon
2017
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Online Access: | http://hdl.handle.net/1794/22692 |