Abstract
In the seismic tomography problem, the subsurface slowness distribution is estimated from the travel-times computed along generally curved rays. For a dense and uniform set of rays, the slowness distribution will be correctly reconstructed. However, for an uneven distribution of rays, the estimated slowness distribution may be influenced by the ray configuration.
© 1998 Optical Society of America
PDF ArticleMore Like This
Erh-Ya Lin, Yao Wang, Yaling Pei, and Randall L. Barbour
ATuD26 Advances in Optical Imaging and Photon Migration (BIOMED) 1998
Tetsuya YUASA, Balasigamani DEVARAJ, Yuuki WATANABE, Takao AKATSUKA, and Humio INABA
ATuD27 Advances in Optical Imaging and Photon Migration (BIOMED) 1998
Bruce D. Cornuelle
SThA.3 Signal Recovery and Synthesis (SRS) 1998