Structure of young East Pacific Rise lithosphere from ambient noise correlation analysis of fundamental- and higher-mode Scholte-Rayleigh waves

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• 作者：Huajian Yao^a ;   ; ^c ;   ; ^{hjyao@mit.edu} ; Pierre Goué ; dard^a ; John A. Collins^b ; Jeffrey J. McGuire^b ; Robert D. van der Hilst^a
• 关键词：East Pacific Rise ; Lithosphere ; Oceanic Uppermost Mantle ; Low-velocity zone ; Ambient noise ; Fundamental- and higher-mode Scholte-Rayleigh waves
• 刊名：Comptes Rendus Geoscience
• 出版年：2011
• 出版时间：September 2011
• 年：2011
• 卷：343
• 期：8-9
• 页码：571-583
• 全文大小：964 K

文摘

Inter-station Green's functions estimated from ambient noise studies have been widely used to investigate crustal structure. However, most studies are restricted to continental areas and use fundamental-mode surface waves only. In this study, we recover inter-station surface (Scholte-Rayleigh) wave empirical Green's function (EGFs) of both the fundamental- and the first-higher mode using one year of continuous seismic noise records on the vertical component from 28 ocean bottom seismographs deployed in the Quebrada/Discovery/Gofar transform faults region on the East Pacific Rise. The average phase-velocity dispersion of the fundamental mode (period band 2?0 s) and the first-higher mode (period band 3? s) from all EGFs are used to invert for the 1-D average, shear-velocity structure in the crust and uppermost mantle using a model-space search algorithm. The preferred shear-velocity models reveal low velocities (4.29 km/s) between Moho and 25 km depth below sea-surface, suggesting the absence of a fast uppermost mantle lid in this young (0? Myr) oceanic region. An even more pronounced low-velocity zone, with shear velocities ?.85 km/s, appears at a depth between 25?0 km below sea-surface. Along with previous results, our study indicates that the shear velocity in the uppermost oceanic mantle increases with increasing seafloor age, consistent with age-related lithospheric cooling.