An Informative Solution to a Seismological Inverse Problem

AUTOR(ES)

Gilbert, Freeman

RESUMO

Preliminary results are presented that infer that 2 sec should be added to the tabular values for P phases and 4 sec to the tabular values for S phases of seismic travel times. From seismic evidence, the radius of the inner core of the Earth is 1229-1250 km; the radius of the outer core is 3482-3485 km. Data are presented relating resolving power with error of measurement for the Earth's mantle.

Documentos Relacionados

• Solution of an inverse problem for fractals and other sets
• General solution to the inverse problem of the differential equation of the ultracentrifuge.
• On an inverse boundary value problem
• A regularized solution with weighted Bregman distances for the inverse problem of photoacoustic spectroscopy
• Optimal Solutions to a Linear Inverse Problem in Geophysics