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Is a lowering of apparent velocity an indicator for rising magma in array seismology? 


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A decrease in apparent velocity can indeed serve as an indicator of rising magma in array seismology. Studies have shown that significant velocity decreases were detected during swarm episodes associated with magma intrusion, with changes exceeding 0.3%. Additionally, the technique of coda wave interferometry has been utilized to identify velocity variations before volcanic eruptions, showcasing complex patterns of apparent velocity variations leading up to eruptions. These variations in seismic velocity have been linked to magmatic intrusions, stress field perturbations, and the migration of magma within volcanic structures. Therefore, monitoring apparent velocity changes through array seismology can provide valuable insights into the dynamics of magma movement and potential volcanic activity.

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Yes, a lowering of apparent slowness in seismic arrays can indicate rising magma, as observed at Deception Island volcano, suggesting the presence of shallow magma chambers and rigid bodies.
Yes, a lowering of apparent velocity can indicate rising magma in array seismology, as observed before the 2010 eruption of Merapi volcano, Java, suggesting magma intrusion and potential volcanic activity.

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