Seismological evidence for differential rotation of the Earth's inner core

被引:338
作者
Song, XD [1 ]
Richards, PG [1 ]
机构
[1] COLUMBIA UNIV,DEPT EARTH & ENVIRONM SCI,NEW YORK,NY 10027
关键词
D O I
10.1038/382221a0
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
The travel times of seismic waves that traverse the Earth's inner core show a small but systematic variation over the past three decades. This variation is best explained by a rotation of the inner core that moves the symmetry axis of its known seismic anisotropy. The inferred rotation rate is on the order of 1 degrees per year faster than the daily rotation of the mantle and crust.
引用
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页码:221 / 224
页数:4
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