Large Silicic Eruptions, Episodic Recharge, and the Transcrustal Magmatic System
Abstract Large silicic eruptions result from rapid evacuation of large, upper crustal reservoirs of silicic magmas. These silicic magmas are thought to be replenished by melt extracted from underlying crystal‐rich source mushes, but the timescales and mechanisms of such melt extraction are unclear....
Sábháilte in:
| Príomhchruthaitheoirí: | , |
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| Formáid: | Artigo |
| Teanga: | Inglês |
| Foilsithe / Cruthaithe: |
Wiley
2020-09-01
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| Sraith: | Geochemistry, Geophysics, Geosystems |
| Ábhair: | |
| Rochtain ar líne: | https://doi.org/10.1029/2020GC009220 |
| Clibeanna: |
Níl clibeanna ann, Bí ar an gcéad duine le clib a chur leis an taifead seo!
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