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- W2023803384 abstract "This paper discusses certain basic problems of tectonophysics studied in our laboratory. Models of folding have been made that lead to methods of calculating the strain due to plastic flow in natural folds. A correlation between the viscosity of plastic flow of crustal rocks and the absorption of seismic waves was found and is used to estimate this viscosity in the crust. The orientation and magnitude of tectonic stress fields in the crust are determined from the polarities of seismic waves, the strain rate of the crust, the energy released by earthquakes, and the strength of materials studied in the laboratory. Different types of deformation observed in the field are discussed both in terms of results of laboratory models and from a theoretical point of view. The influence of pre-existing faults on the stress field is studied with laboratory modeling." @default.
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- W2023803384 date "1972-01-01" @default.
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- W2023803384 title "Tectonophysical characteristics of stresses, slow deformation in the Earth's crust, and the earthquake mechanism" @default.
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- W2023803384 doi "https://doi.org/10.1016/0031-9201(72)90007-6" @default.
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