Titlebook: Upper Mantle Heterogeneities from Active and Passive Seismology; Karl Fuchs Book 1997 Springer Science+Business Media Dordrecht 1997 explo

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Problems of Active Seismologymic processes and rheological characteristics of anomalous zones of earthquake preparation. Since nuclear explosions are prohibited, the vibroseismic method is the only active method for deep Earth’s sounding [1], [2].

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Heterogeneity of the Uppermost Eurasian Mantle along the DSS Profile “Quartz”, Russiamical explosions. Our interpretation shows a 42-kin thick, high-velocity crust under the Baltic Shield, a 29-km thick crust and high-velocity upper mantle under the Mezenskaya depression, 52-km thick crust with high-velocity lower crust and uppermost mantle under the Urals, and 40-km thick crust und

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Joint Inversion of Teleseismic Delay Times and Gravity Anomaly Data for Regional Structuresnship between density and velocity anomalies exists, the value of which is unknown and may vary in different regions of the model, especially with depth. Therefore, the correlation coefficient is treated as additional unknown parameter, leading to a non-linear (quasi Gaussian) inversion scheme. The

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Teleseismic Tomography in Sweden-Denmark-Germany, Project TORthe transition between Proterozoic and Paleozoic Europe, the most prominent geological border line in Europe. It runs through Denmark, Sweden, Poland, Ukraine and Romania and is expected to show large lithospheric differences, based on previous studies. The project goes to depths of 200–300 km. The

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The 1995 U.S. Deep Probe Project1.25 km intervals along a roughly north-south line which extended along the North American Cordillera and across the Alberta plains from southern New Mexico to Edmonton, Alberta. The experiment has revealed profound differences in the structure of the crust and upper mantle north and south of the ea

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