A Surface Wave Study of the South-China Subplate
Abstract
New data from the Seismological Research Observatory (SRO) is used in conjunction with a non-linear least squares technique to invert surface wave group velocity data for the shear velocity structure of the South-China subplate. A multi-filter analysis was used to produce group velocities for the fundamental mode Love and Rayleigh wave. A number of earthquakes over a single path are used in order to deduce a measure of the observational uncertainty of the present method. Group velocity standard deviations range from .03 to .1 km/ sec for Love waves over the period range of 10 to 65 seconds. Results of the inversion indicate that a 3 layer, 40 km thick crust is an adequate model consistent with the data for the South-China subplate. Crustal shear velocities are found to be higher and upper mantle shear velocities lower than previously reported values for this region.
Document Details
- Document Type
- Technical Report
- Publication Date
- Aug 01, 1977
- Accession Number
- ADA126498
Entities
People
- Ta-liang Teng
Organizations
- University of Southern California