:湿?

Marc Hirschmann1

  • 1Department of Geology and Geophysics, University of Minnesota, Minneapolis, Minnesota 55455, USA. marc.m.hirschmann-1@umn.edu

Nature
|January 27, 2006
PubMed
概括

地球地幔过渡区可能不会像以前认为的那样容纳大量的水. 降低条件,而不是高含水量,可能解释了它的电导率,影响了地球动力学和地球化学.

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