Constraining Crustal Volatile Release in Magmatic Conduits by Synchrotron X-ray μ-CT
Magma-crust interaction in magma reservoirs and conduits is a crucial process during magma evolution and ascent. This interaction is recorded by crustal xenoliths that frequently show partial melting, inflation and disintegration textures. Frothy xenoliths are widespread in volcanic deposits from al...
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| Format: | Others |
| Language: | English |
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Uppsala universitet, Berggrundsgeologi
2011
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| Online Access: | http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-160230 |