The movement of tectonic plates leads to strain build-up in the Earth, which can be released
during earthquakes when one side of a seismic fault suddenly slips with respect to the other …

The source mechanism of 19 earthquakes that occurred in Peru (1990–1996) is studied
using broad band data. Focal mechanisms are obtained using polarities of P wave and body …

This study investigates the spatial and temporal distribution of energy release of large,
intermediate‐depth earthquakes using a modified back projection technique first used to …

We analyze 17 intermediate-depth, normal-faulting, inslab earthquakes of Mexico (4.1≤ M
w≤ 7.4; 35 km≤ H≤ 118 km), recorded on hard sites at local and regional distances (R≤ …

To constrain dynamic source properties of deep earthquakes, we have systematically
constructed broadband time functions of deep earthquakes by stacking and scaling …

Earthquake source time functions deconvolved from teleseismic broadband P wave
recordings are used to examine rupture variations for 417 underthrusting earthquakes …

Rupture properties, such as rupture direction, length, propagation speed and source
duration, provide important insights into earthquake mechanisms. One approach to estimate …

The systematic behavior of earthquake rupture as a function of earthquake magnitude
and/or tectonic setting is a key in our understanding of the physical mechanisms involved …

We developed an inversion algorithm to determine the Source Time Function and Moment
Tensor of intermediate and deep earthquakes from a set of teleseismic body wave records …

We have compiled source-time functions (STFs) of 54 Mexican earthquakes (3.0≤ M≤ 8).
The depth, H, of 48 of these earthquakes lies between 10 and 50 km. The STFs of 43 …