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Regional seismograms are dominated by the phases Pn, Pg, Sn, and Lg. More often Sn and Lg are used to infer the attenuation structure of the lithosphere. The seismic phase Sn is a high-frequency shear-wave (typically from 1 to 4 Hz and occasionally higher) that travels in the lithospheric mantle above the negative velocity gradient which usually marks the lithosphere-asthenosphere boundary. Sn has been reported out to distances of 35° (e. g. , MO...
By H.J. Patton
Series: Pageoph Topical Volumes
Paperback: 228 pages
Publisher: Birkhäuser; 2001 edition (September 21, 2001)
Language: English
ISBN-10: 3764365501
ISBN-13: 978-3764365509
Product Dimensions: 7 x 0.6 x 10 inches
Amazon Rank: 16890005
Format: PDF ePub djvu book
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