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seismic discontinuity |
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seismic discontinuity [′sīz·mik ‚dis·känt·ən′ü·əd·ē]
(geophysics) A surface at which velocities of seismic waves change abruptly. A boundary between seismic layers of the earth. Also known as interface; velocity discontinuity. Want to thank TFD for its existence? Tell a friend about us, add a link to this page, add the site to iGoogle, or visit the webmaster's page for free fun content. |
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