Geophysical imaging (also known as geophysical tomography) is a minimally destructive geophysical technique that investigates the subsurface of a terrestrial planet.[2][3] Geophysical imaging is a noninvasive imaging technique with a high parametrical and spatio-temporal resolution.[4] It can be used to model a surface or object understudy in 2D or 3D as well as monitor changes.[4]
^S. R., Kiran (2017). "General Circulation & Principal Wave Modes in Andaman Sea from Observations". SSRN Working Paper Series. doi:10.2139/ssrn.3072272. ISSN1556-5068.
^Parsekian, A. D.; Singha, K.; Minsley, B. J.; Holbrook, W. S.; Slater, L. (2015). "Multiscale geophysical imaging of the critical zone: Geophysical Imaging of the Critical Zone". Reviews of Geophysics. 53 (1): 1–26. doi:10.1002/2014RG000465.
^Afonso, Juan Carlos; Moorkamp, Max; Fullea, Javier (2016), "Imaging the Lithosphere and Upper Mantle", Integrated Imaging of the Earth, John Wiley & Sons, Inc, pp. 191–218, doi:10.1002/9781118929063.ch10, ISBN9781118929063