High-resolution seismic constraints on flow dynamics in the oceanic asthenosphere

被引:0
|
作者
Pei-Ying Patty Lin
James B. Gaherty
Ge Jin
John A. Collins
Daniel Lizarralde
Rob. L. Evans
Greg Hirth
机构
[1] Lamont-Doherty Earth Observatory of Columbia University,Department of Geology and Geophysics
[2] Woods Hole Oceanographic Institution,Geological Sciences Department
[3] Brown University,undefined
[4] †Present address: Taiwan Ocean Research Institute,undefined
[5] National Applied Research Laboratories,undefined
[6] Kaohsiung,undefined
[7] Taiwan (P.-Y.P.L.).,undefined
来源
Nature | 2016年 / 535卷
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摘要
Rayleigh waves recorded with an ocean-bottom seismograph array in the central Pacific Ocean constrain the seismic anisotropy within the oceanic lithosphere–asthenosphere system: seafloor-spreading-induced lithospheric fabric generates the strongest anisotropy, while density- and/or pressure-driven flow produces a secondary peak in anisotropy at the base of the asthenosphere.
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页码:538 / 541
页数:3
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