Lateral variations of seismic-wave attenuation in the upper mantle above the inclined earthquake zone of the Tonga Island Arc: Deep anomaly in the upper mantle

Author:

Barazangi Muawia,Isacks Bryan

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference76 articles.

1. Generation and propagation of G waves from the Niigata earthquake of June 16, 1964, 2, Estimation of earthquake moment, released energy, and stress-strain drop from G wave spectrum;Aki;Bull. Earthquake Res. Inst. Tokyo Univ.,1966

2. Allen , C. R. T. Matsuda A. Okada Relationship between seismicity and geologic structure in western Japan 1970

3. The anelasticity of the earth;Anderson;J. Geophys. Res.,1964

4. Attenuation in the mantle and rigidity of the core from multiply reflected core phases;Anderson;Proc. Nat. Acad. Sci. U.S.,1964

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