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Updated: Nov 18, 2025

Stress Distribution During Cold Compression of Rocks and Mineral Aggregates Using Synchrotron-based X-Ray Diffraction
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地震の大きさの分布の変動は,異なるストレス体制によって異なります

Danijel Schorlemmer1, Stefan Wiemer, Max Wyss

  • 1Swiss Seismological Service, ETH Zürich, ETH Hönggerberg, Schafmattstr. 30, 8093 Zürich, Switzerland. danijel@sed.ethz.ch

Nature
|September 24, 2005
PubMed
まとめ

b値で測定される地震の大きさの分布は,断層スタイルによって異なります. 通常の故障は高いb値を示し,推力故障は低いb値を示し,b値がストレスメーターとして機能することを示します.

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