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Updated: Jul 13, 2026

Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling
06:55

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Published on: August 5, 2016

マントルの底辺にある至る所に存在する地震の不連続性の証拠です

Sidorin1, Gurnis, Helmberger

  • 1Seismological Laboratory 252-21, California Institute of Technology, Pasadena, CA 91125, USA.

Science (New York, N.Y.)
|November 13, 1999
PubMed
まとめ

地震学的な研究は,地球のマントルの底辺の不連続性を示唆しています. この断絶は,おそらく相変化であり,コア-マントルの境界線より200km上にある.

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