Eruption versus intrusion? : arrest of propagation of constant volume, buoyant, liquid-filled cracks in an elastic, brittle host
When a volume of magma is released from a source at depth, one key question is whether or not this will culminate in an eruption or in the emplacement of a shallow intrusion. We address some of the physics behind this question by describing and interpreting laboratory experiments on the propagation...
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Main Authors: | , |
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Format: | Article |
Language: | English |
Published: |
2012
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Subjects: | |
Online Access: | https://hdl.handle.net/10356/94848 http://hdl.handle.net/10220/8401 |
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Institution: | Nanyang Technological University |
Language: | English |
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