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Institute of Earthquake Prediction Theory and Mathematical Geophysics

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Global Geodynamic Model of the Earth and Its Application to the Arctic Region

Number of Aftershocks in Epidemic-type Seismicity Models and reality

The Deepest Depressions on Land in Antarctica as a Result of Cenosoic Riftogenesis Activation

Thermal state of the lithosphere beneath The Laptev Sea: Geodinamic implications from geomagnetic data

Potential Locations of Strong Earthquakes in Bulgaria and the Neighbouring Regions

The largest earthquakes in subduction zones around the Polar Regions.

Inverse scattering – Fourier analysis – super-resolution

Structure of the seismic field of the baikal rift zone

Trigger mechanisms of gas hydrate decomposition, methane emissions and glacier breakup in polar regions as the result of deformation tectonic waves

Productivity within the epidemic-type seismicity model

Nonlinear large-scale perturbations of steady thermal convective dynamo regimes in a plane layer of electrically conducting fluid rotating about the vertical axi

Inverse scattering – Fourier analysis – phase retrieval

A strip with constant stresses on the cut: exact solutions

Approaches to Solving the Maximum Possible Earthquake Magnitude (Mmax) Problem

A TEMPERATURE PROBLEM FOR A SQUARE: AN EXACT SOLUTION

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