Seismic Velocity Structure Beneath Kirishima Volcanoes with Differential Analysis of Explosion Experiment
Seismic velocity structures beneath Kirishima volcanoes are estimated down to 3 km from the surface with the differential analysis of refraction from the explosion experiment. Three layers are interpreted in the central and northern part of the volcanoes and two layers are interpreted in the souther...
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Veröffentlicht in: | BULLETIN OF THE VOLCANOLOGICAL SOCIETY OF JAPAN 1996/11/30, Vol.41(5), pp.227-241 |
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Format: | Artikel |
Sprache: | jpn |
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