Regional patterns of present-day tectonic stress can be used to evaluate the forces acting on
the lithosphere and to investigate intraplate seismicity. Most intraplate regions are …

An array of graphical and numerical techniques facilitate qualitative and quantitative
kinematic analysis of fault-slip data. Graphical contouring and Bingham statistics of the …

A new method for determining the reduced stress tensor with four degrees of freedom (the
orientations of the three principal stress axes as well as the ratio of principal stress …

The inversion of earthquake focal mechanisms is one of the few tools available for
determining principal stress directions at seismogenic depths. Various methods have been …

В монографии с позиций тектонофизики обобщены результаты изучения строения,
механизмов формирования и эволюции разрывных сетей в разноранговых разломных …

Program FMSI inverts observations of slip directions on fault planes of known orientation in
order to determine the best-fitting four-parameter stress tensor, defined by three principal …

3.1. 2.1 Macroseismic intensity 13 3.1. 2.2 Magnitude and early relationships to seismic
energy 13 3.1. 2.3 Scalar seismic and geometric moment, source spectrum, source …

Using detailed microearthquake data, we present a stress tensor inversion scheme with new
methods for selecting the fault planes and allowing for errors in the focal mechanisms. The …

The shear stress direction on a fault plane depends only on four of the six components of the
stress tensor. Assuming only that the slip direction marks the shear stress direction on any …

The middle to late Cenozoic tectonic-magmatic evolution of the Sierra Madre Occidental
volcanic province south of the Tropic of Cancer is summarized and analyzed for the first …