Measurement ofQfor very long period free oscillations

Author:

Alsop Leonard E.,Sutton George H.,Ewing Maurice

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

Reference8 articles.

1. Free oscillations of the earth observed on strain and pendulum seismographs;Alsop;J. Geophys. Research,1961

2. The rotational splitting of the free oscillations of the earth;Backus;Proc., National Acad. Sci.,1961

3. Excitation of the free oscillations of the earth by earthquakes;Benioft;J. Geophys. Research,1961

4. Attenuation of dispersed wave trains;Brune;Bull. Seism. Soc. Am.,1961

5. Mantle Rayleigh waves from the Kamchatka earthquake of November 4, 1952;Ewing;Bull. Seism. Soc. Am.,1954

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1. The Damping of S Waves;Geophysical Journal of the Royal Astronomical Society;2010-01-26

2. Q measurements for PhaseX overtones;Pure and Applied Geophysics PAGEOPH;1990

3. Shear velocity and shear attenuation models inverted from the world-wide and pure-path average data of mantle Rayleigh waves (0S25 to 0S80) and fundamental spheroidal modes (0S2 to 0S24);Geophysical Journal International;1981-07-01

4. Free Oscillations of the Earth;Annual Review of Earth and Planetary Sciences;1981-05

5. Q−1 models from data space inversion of fundamental spheroidal mode attenuation measurements;Anelasticity in the Earth;1981

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