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在东北太平洋上升下被动地幔上升的电图

Kerry Key1, Steven Constable, Lijun Liu

  • 1Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography, University of California, San Diego, La Jolla, California 92093, USA. kkey@ucsd.edu

Nature
|March 30, 2013
PubMed
概括

板块构造驱动地幔上升,在中洋山脊上形成海洋地. 新的地质物理数据显示,在东太平洋上升处主导的是被动上升,融化聚焦发生在多孔融化区域.

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