Results 71 to 77 of about 105 (77)
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Tectonophysics, 1974
Abstract Physical theory and laboratory experiments both indicate that tectonomagnetic effects in seismically active areas should be detected with highly sensitive drift-free differential magnetometers. By using a pair of synchronized 0.25 7 absolute magnetometers to measure precisely field differences between 70 adjacent sites with a 10–15 km ...
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Abstract Physical theory and laboratory experiments both indicate that tectonomagnetic effects in seismically active areas should be detected with highly sensitive drift-free differential magnetometers. By using a pair of synchronized 0.25 7 absolute magnetometers to measure precisely field differences between 70 adjacent sites with a 10–15 km ...
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Izvestiya, Physics of the Solid Earth, 2016
Plate tectonics only allows small deformations in the lithospheric plates. The laboratory experiments with the rock specimens show that the creep is transient when the creep strain is at most 1%. Hence, if we assume that the creep strain in the lithospheric plates is below this threshold, the creep is transient.
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Plate tectonics only allows small deformations in the lithospheric plates. The laboratory experiments with the rock specimens show that the creep is transient when the creep strain is at most 1%. Hence, if we assume that the creep strain in the lithospheric plates is below this threshold, the creep is transient.
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Tectonomagnetic Monitoring of the Wilhelm Archipelago in the Argentine Islands Area
International Conference of Young Professionals «GeoTerrace-2022», 2022V. Maksymchuk +4 more
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Informativity Of Tectonomagnetic Monitoring In The Transcarpathians Active Seismic Zone
Proceedings, 2018V. Maksymchuk +4 more
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On tectonomagnetic effects in a seismic area
1981BOZZO E., CANEVA A., PASQUALE, VINCENZO
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The model of tectonomagnetic effect formation in the fracture zone with shear
Russian Journal of Earth Sciences, 1998openaire +1 more source

