Explore: Seismic Tomography

Seismic tomography or seismotomography is a technique for imaging the subsurface of the Earth using seismic waves. The properties of seismic waves are

rifts can be grouped into the techniques of isotope geochemistry, seismic tomography and geodynamical modeling. The varying geochemical signatures of a

Tomography is imaging by sections or sectioning that uses any kind of penetrating wave. The method is used in radiology, archaeology, biology, atmospheric

including seismic methods, electrical resistivity tomography, ground-penetrating radar, etc. Types of geophysical imaging: Electrical resistivity tomography Ground-penetrating

characterized by slow shear wave velocities and were discovered by seismic tomography of deep Earth. There are two main provinces: the African LLSVP and

commonly cited seismic wave-speed images that are used to look for variations in regions where plumes have been proposed come from seismic tomography. This method

properties using seismology, petrology, isotope geochemistry and seismic tomography techniques. Seismology in particular is heavily relied upon for information

surface. Seismic records have been used to map the torn slabs beneath the Caucasus continental – continental convergence zone, and seismic tomography has mapped

continuing the legacy of the WWSSN. The advancement in seismic tomography and the expansion of the Global Seismic Network, alongside greater computational power

phenomenon, which has been imaged by seismic tomography. There is a concentration of velocity anomalies in the tomography that is thicker than the slab itself