the rheology of the earth in the intermediate time range
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ID: 151993
1970
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Abstract
The evidence bearing upon the rheology of the " tectonically<br />significant layers" of the Earth (" tectonosphere ") in the intermediate<br />time range (4 hours to 15000 years) is analyzed. This evidence is<br />based upon observations of rock-behavior in the laboratory, of seismic<br />aftershock sequences, of Earth tides and of the decay of the Chandler wobble.<br />It is shown that of the rheological models (Maxwell-material, Kelvin-material,<br />and logarithmically creeping material) advocated in the literature, only that<br />based on logarithmic creep does not contradict any of the observational<br />evidence available to date. In addition, a strength limit may be present.
| Reference Key |
scheidegger1970annalsthe
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|---|---|
| Authors | ;A. E. SCHEIDEGGER |
| Journal | desalination |
| Year | 1970 |
| DOI |
10.4401/ag-5141
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| URL | |
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