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DOI10.1126/science.1228194
Body-wave imaging of Earth's mantle discontinuities from ambient seismic noise
Poli P.; Campillo M.; Pedersen H.
发表日期2012
ISSN0036-8075
起始页码1063
结束页码1065
卷号338期号:6110
英文摘要Ambient seismic noise correlations are widely used for high-resolution surface-wave imaging of Earth's lithosphere. Similar observations of the seismic body waves that propagate through the interior of Earth would provide a window into the deep Earth. We report the observation of the mantle transition zone through noise correlations of P waves as they are reflected by the discontinuities associated with the top [410 kliometers (km)] and the bottom (660 km) of this zone. Our data demonstrate that high-resolution mapping of the mantle transition zone is possible without using earthquake sources.
英文关键词ambient noise; body wave; correlation; lithosphere; mantle; mantle discontinuity; P-wave; seismic noise; transition zone; wave propagation; ambient seismic noise; article; body wave imaging; earthquake; environmental monitoring; geography; geology; imaging; lithosphere; noise; priority journal
语种英语
来源期刊Science
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/245103
作者单位Institut des Sciences de la Terre (ISTerre), Universitéde Grenoble I, CNRS, BP 53, F-38041 Grenoble Cedex 9, France
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Poli P.,Campillo M.,Pedersen H.. Body-wave imaging of Earth's mantle discontinuities from ambient seismic noise[J],2012,338(6110).
APA Poli P.,Campillo M.,&Pedersen H..(2012).Body-wave imaging of Earth's mantle discontinuities from ambient seismic noise.Science,338(6110).
MLA Poli P.,et al."Body-wave imaging of Earth's mantle discontinuities from ambient seismic noise".Science 338.6110(2012).
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