Surface Waves, Seismic Refraction and Upper Mantle Structure of the Basin and Range

Abstract

Earlier study of Great Basin structure using surface waves have been extended to include the Southern Basin and Range of Arizona, and the Volcanic Plateau of Northern Nevada and Southern Oregon. The crust of the Southern Basin and Range is slightly thinner than that of the Great Basin while the mantle structure is similar. The Volcanic Plateau has a thicker crust (based on refraction data) than the Great Basin while the mantle lid zone is either thin or absent. (Author)

Open PDF

Document Details

Document Type
Technical Report
Publication Date
Jan 20, 1980
Accession Number
ADA088752

Entities

People

  • Keith F. Priestley

Organizations

  • University of Nevada, Reno

Tags

Communities of Interest

  • Energy and Power Technologies

DTIC Thesaurus Topics

  • Agreements
  • California
  • Dispersions
  • Earth Models
  • Excitation
  • Geophysics
  • Group Velocity
  • Heat Transmission
  • North America
  • Observation
  • Phase Velocity
  • Rayleigh Waves
  • Refraction
  • Secondary Waves
  • Surface Waves
  • United States
  • Waves

Fields of Study

  • Geology

Readers

  • Seismology