COLLECTION AND ANALYSIS OF SEISMIC-WAVE PROPAGATION DATA

Abstract

The report discusses the results of an extensive long-range reversed refraction profile which traverses the Michigan Basin and the Appalachian Mountains. Particular emphasis is placed on the attenuation of first compressional wave arrivals and on crustal-upper mantle structure. Also included are results of a survey on lake bottom seismic background noise in Lake Superior. Although large signal levels were obtained in the lake bottom, long periods of high background noise indicated that land based seismographs are superior. Theoretical studies in elastic wave scattering were made to evaluate the effect of nonhomogeneities on the propagation of elastic waves. Theoretical development of mode filtering (previously demonstrated empirically), is nearly completed. A LASA digital data convertor was designed, constructed, and put into operation. Two- and three-dimensional seismic ray-tracing techniques using digital modeling were developed. These techniques enable the seismologist to determine the effects of lateral inhomogeneities and irregularities in velocity interfaces on travel time and attenuation of seismic waves.

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Document Details

Document Type
Technical Report
Publication Date
Sep 01, 1968
Accession Number
AD0675057

Entities

People

  • David E. Willis
  • Philip L. Jackson

Organizations

  • University of Michigan

Tags

Communities of Interest

  • Energy and Power Technologies

DTIC Thesaurus Topics

  • Appalachian Mountains
  • Background Noise
  • Computer Programs
  • Computers
  • Diffraction
  • Digital Data
  • Elastic Waves
  • Geometry
  • Lake Superior
  • Mountains
  • Ray Tracing
  • Scattering
  • Seismic Waves
  • Three Dimensional
  • Travel Time
  • United States
  • Wave Propagation

Readers

  • Atmospheric Science / Meteorology, specifically Wind Wave Turbulence.
  • Seismology