CaSiO3の地震速度は,地球の下層マントルのLLSVPを説明することができます

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Updated: Apr 30, 2026

Data Processing Methods for 3D Seismic Imaging of Subsurface Volcanoes: Applications to the Tarim Flood Basalt
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Data Processing Methods for 3D Seismic Imaging of Subsurface Volcanoes: Applications to the Tarim Flood Basalt

Published on: August 7, 2017

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A R Thomson1,2, W A Crichton3, J P Brodholt4,5

  • 1Department of Earth Sciences, University College London, London, UK. a.r.thomson@ucl.ac.uk.

Nature
|August 16, 2019
PubMed
まとめ

下層マントルの重要な鉱物であるカルシウムシリケートペロブスキットは,予想より低い切断モジュールを持っています. この発見は,海底の地殻が地震速度の異常を引き起こし,大きな低シェア速度の州を説明することを示唆しています.

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