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Karsten Bahr1, Fiona Simpson

  • 1Geophysics Institute, University of Göttingen, 37075 Göttingen, Germany. kbahr@uni-geophys.gwdg.de

Science (New York, N.Y.)
|February 16, 2002
PubMed
概括

橄中的扩散解释了上层地幔的导电性. 电动异质性测量表明地幔对流,而不是板块运动,导致费诺斯坎迪亚板块和澳大利亚板块下方的奥利文线对齐.

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