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Updated: Jul 9, 2026

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地震の速度と密度は,410キロメートルと660キロメートルの不連続度を越えてジャンプします

Shearer1, Flanagan

  • 1Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography, University of California, San Diego, La Jolla, CA 92093-0225, USA. Lawrence Livermore National Laboratory, Post Office Box 808, L-206, Livermore, CA 94551, USA.

Science (New York, N.Y.)
|September 8, 1999
PubMed
まとめ

地震波の分析により,上部マントルの不連続性に関する新たな制約が明らかになった. 660キロメートルの不連続は,以前にモデリングされたよりも小さな密度ジャンプを示し,マントルのコンベクション研究に影響を与えています.

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