Timescales of magma ascent during explosive eruptions: Insights from the re-equilibration of magmatic volatiles
The explosivity of volcanic eruptions is governed in part by the rate at which magma ascends and degasses. Because the timescales of eruptive processes can be exceedingly fast relative to standard geochronometers, magma ascent rate remains difficult to quantify. As an exception to this principle, ma...
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| Language: | English |
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2014
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| Online Access: | https://doi.org/10.7916/D8F769QW |