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・ Seismic Micro-Technology
・ Seismic microzonation
・ Seismic migration
・ Seismic moment
・ Seismic noise
・ Seismic rail sensing
・ Seismic refraction
・ Seismic response of landfill
・ Seismic retrofit
・ Seismic risk
・ Seismic scale
・ Seismic Seconds
・ Seismic site effects
・ Seismic source
・ Seismic to simulation
Seismic tomography
・ Seismic trace
・ Seismic Unix
・ Seismic vibrator
・ Seismic wave
・ Seismicity of the Sanriku coast
・ Seismicity of the Sumatra coast
・ Seismite
・ Seismo Creek
・ Seismo-electromagnetics
・ Seismoelectrical method
・ Seismogenic layer
・ Seismogram
・ Seismological Society of America
・ Seismological Society of Japan


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Seismic tomography : ウィキペディア英語版
Seismic tomography
Seismic tomography is a technique for imaging Earth’s sub-surface characteristics in an effort to understand deep geologic structure. Gathering ample compressional wave (P-wave) and transverse wave (S-wave) travel time measurements allows us to compile 3D images of earth’s velocity structure.
==Theory==
Tomography is solved as an inverse problem. First measurements are made of seismic waves passing through a material. The character of these measurements is then analyzed to make inferences on the material such waves have passed through (velocity, density, etc.).〔(【引用サイトリンク】url=http://www.landtech.org/pdf/pdf1.pdf )〕 The velocity of p and s waves depends on the rheology of the material that they travel through (density and elasticity). In short, variations in chemical compositions and thermal structure result in a change of velocity. Such waves can travel faster through relatively colder material.〔〕 It is observed that wave velocity increases with increasing depth from 2–8 km/s in the crust up to 13 km/s in the mantle. Current research is based on this premise.

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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