Abstract
Summary The splitting matrix for a set of coupled multiplets is a linear combination of structure coefficients, first-order Coriolis terms and terms for ellipticity and centrifugal force. These latter terms are calculated for a good 1-D earth model and removed. The first-order Coriolis terms are then uniquely determined. They are linear functionals of the density of the 1-D model. The remaining splitting matrix is an orthogonal transformation of the structure coefficients. The inverse orthogonal transformation is easily constructed and the set of structure coefficients is then obtained linearly from the splitting matrix. The structure coefficients are linear functionals of 3-D structure.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
