Simultaneous Inversion of cross-dipole acoustic waveforms in anisotropic media for azimuthal angle and dispersion of fast and slow shear waves

A method to jointly invert for azimuthal angle and dispersion relations from cross-dipole data is presented. Dispersion curves from the joint inversion are compared to both Prony’s method and a simple back propagation schema and an agrrement is found. The azimuthal angle estimate is shown to differ...

Cur síos iomlán

Sonraí bibleagrafaíochta
Príomhchruthaitheoirí: Briggs, Victoria, Rao, Rama V. N., Burns, Daniel R.
Rannpháirtithe: Massachusetts Institute of Technology. Earth Resources Laboratory
Formáid: Technical Report
Foilsithe / Cruthaithe: Massachusetts Institute of Technology. Earth Resources Laboratory 2011
Rochtain ar líne:http://hdl.handle.net/1721.1/67859
Cur síos
Achoimre:A method to jointly invert for azimuthal angle and dispersion relations from cross-dipole data is presented. Dispersion curves from the joint inversion are compared to both Prony’s method and a simple back propagation schema and an agrrement is found. The azimuthal angle estimate is shown to differ from a frequency domain rotaion that takes no account of dispersion within the waveforms indicating the importance of joint inversion.