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Observations from multiple seiche load induced transient strains constrain the upper crustal magma reservoir beneath Yellowstone Caldera.
Observations from multiple seiche load induced transient strains constrain the upper crustal magma reservoir beneath Yellowstone Caldera.
2016
K. J. Gryger
K. M. Luttrell
Keywords:
Magma
Seiche
Volcanology
Caldera
Geology
Petrology
Correction
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