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Hiroki Sato, Kenichi Muro
Department of Earth and Space Science, Osaka University,
Toyonaka, Osaka 560-0043, Japan
roki@ess.sci.osaka-u.ac.jp

Akira Hasegawa
Research Center for Prediction of Earthquakes and Volcanic Eruptions,
Tohoku University, Sendai 980-0845, Japan.

Seismic tomographic studies have determined three-dimensional (3D) velocity structures, in detail, of the crust and the upper mantle of the Earth. Yet, simple two-dimensional (2D) sections have generally been used to present 3D tomographic results. Here we show 3D views and animations of the Earth's structure that are made as easy as 2D sections by using Mathematica. As an example, low-velocity zones in the upper mantle are shown in three dimensions together with major volcanoes, mid-crustal reflectors, earthquake hypocenters, the Moho discontinuity, and the upper plane of the subducted slab that are observed in northeastern Japan. Low velocities in volcanic areas generally correspond to high temperature and indicate possible presence of magma. The 3D animations enable us to investigate the special correlation between low-velocity zones, volcanoes, reflectors, earthquakes, and the slab, and thus enable us to study magma ascent pathways in detail.

Introduction

3D Structure and Animation

Distribution of Volcanoes and Hot Low-Velocity Zones, and Mantle Dynamics

Summary

Acknowledgments

References

Additional Material


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