1962Journal of Geophysical Research AtmospheresRequires access

Release of tectonic strain by underground nuclear explosions

Frank Press, C. B. Archambeau

Open publisher page 87 citations

Abstract

The strong excitation of SH waves and other phenomena associated with underground nuclear explosions suggest the hypothesis that pre-existing tectonic strain was released by the explosion. The pertinent evidence from the Rainier explosion is reviewed. A calculation of tectonic energy release is made for a simple model in which a spherical cavity is inserted in a prestrained medium. It is tentatively concluded that, although tectonic release does occur, its magnitude is probably too small to affect the character of seismograms. Experiments are suggested which could provide the basis for a better evaluation of the hypothesis.

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What this paper is about

The strong excitation of SH waves and other phenomena associated with underground nuclear explosions suggest the hypothesis that pre-existing tectonic strain was released by the explosion. The pertinent evidence from the Rainier explosion is reviewed. A calculation of tectonic energy release is made for a simple model in which a spherical cavity is inserted in a prestrained medium. It is tentatively concluded that, although tectonic release does occur, its magnitude is probably too small to affect the character of seismograms. Experiments are suggested which could provide the basis for a better evaluation of the hypothesis.

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OpenAlex reports 87 citations for this work. Citation counts describe recorded attention and do not establish research quality.

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Available abstract

The strong excitation of SH waves and other phenomena associated with underground nuclear explosions suggest the hypothesis that pre-existing tectonic strain was released by the explosion. The pertinent evidence from the Rainier explosion is reviewed. A calculation of tectonic energy release is made for a simple model in which a spherical cavity is inserted in a prestrained medium. It is tentatively concluded that, although tectonic release does occur, its magnitude is probably too small to affect the character of seismograms. Experiments are suggested which could provide the basis for a better evaluation of the hypothesis.

Key concepts: Geology, Tectonics, Seismology, Strain (injury), Geophysics, Medicine, Internal medicine

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