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David Bercovici1, Yanick Ricard2
1Department of Geology and Geophysics, Yale University, New Haven, Connecticut 06520-8109, USA.
在地球上,板块构造的启动涉及到10亿年的滞后. 石质层损伤,地幔流动和原沉降结合形成弱板边界,使全球构造学成为可能.
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