日本の地殻構造の特徴
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概要
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Several evidences are presented to support the hypothesis that the asthenosphere low velocity channel reaches to the M discontinuity in Japan. Informations from gravity, refraction and phase velocity studies are combined in a comparison of crust-upper mantle structure in Japan with those in other regions where the velocity beneath the M discontinuity is also lower than normal.
- 社団法人 東京地学協会の論文