,西

P G Silver1, W E Holt

  • 1Department of Terrestrial Magnetism, Carnegie Institution of Washington, Washington, DC 20015, USA. silver@dtm.ciw.edu

Science (New York, N.Y.)
|February 9, 2002
PubMed
まとめ

北米西部の下のマントルの流れは,プレート運動に反対して東に移動します. この弱い結合は,おそらく古代のファラロンプレートからの深層マントルの密度の変動が,流れを駆動することを示唆しています.

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