Volatile loss from melt inclusions in pyroclasts of differing sizes
We have investigated the loss of H 2 O from olivine-hosted melt inclusions (MIs) by designing an experiment using tephra samples that cooled at different rates owing to their different sizes: ash, lapilli, and bomb samples that were deposited on the same day (10/17/74) of the sub-Plinian eruption of...
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Veröffentlicht in: | Contributions to mineralogy and petrology 2013-01, Vol.165 (1), p.129-153 |
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