A Surface Wave Dispersion Study of the Crustal and Mantle Structure of China
Abstract
A measurement procedure was designed which can determine the group velocity with both good resolution and small systematic errors. This technique is being employed in a surface-wave study of the Eurasian continent. The generalized linear inversion theory is applied to obtain pure-path regional dispersion from mixed-path observations. Crust and upper mantle structure of the Eurasian continent is being interpreted with special emphasis on lateral heterogeneities.
Document Details
- Document Type
- Technical Report
- Publication Date
- Jun 01, 1980
- Accession Number
- ADA103087
Entities
People
- Ta-liang Teng
Organizations
- University of Southern California