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- [2] JACOBS JA, 1959, PHYSICS GEOLOGY
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- [4] 1967, GEOPHYS J ROY ASTRO, P14
2-COMPONENT FLOW MODEL FOR CONVECTION IN EARTHS UPPER MANTLE
被引：70
作者：
FRANK, FC
机构：
来源：
关键词：
D O I：
10.1038/220350a0
中图分类号：
O [数理科学和化学];
P [天文学、地球科学];
Q [生物科学];
N [自然科学总论];
学科分类号：
07 ;
0710 ;
09 ;
摘要：
A model for convection in the upper mantle of the Earth comprising two flows, one of percolating melt fluid (which need be no more than a small volume fraction in the intergranular channels of coherent solid matter), the other a solid plastic flow, avoids some paradoxical features of other models for mantle convection. This model leads to a reasonably consistent account of the processes of continental drift. © 1968 Nature Publishing Group.
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页码：350 / &
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