Since 1991, induced earthquakes have been observed and linked to gas production in the
Groningen field. Recorded waveforms are complex, resulting partly from a Zechstein salt …

We present a probabilistic seismic point source inversion, taking into account 3‐D
heterogeneous Earth structure. Our method rests on (1) reciprocity and numerical wavefield …

Determining the seismic moment tensor (MT) from the observed waveforms with available
Earth's structure models is known as seismic waveform MT inversion. It remains challenging …

Characterizing seismic moment tensors of small‐to moderate‐magnitude earthquakes (ie,
2.5< M< 4.0) still represents a challenge in observational seismology. To address this …

Although both earthquake mechanism and 3‐D Earth structure contribute to the seismic
wavefield, the latter is usually assumed to be layered in source studies, which may limit the …

We have developed a new, fully automated tool for the centroid moment tensor (CMT)
inversion in a Bayesian framework. It includes automated data retrieval, data selection …

A seismic moment tensor is a 3× 3 symmetric matrix that provides a compact representation
of a seismic source. We develop an algorithm to estimate moment tensors and their …

Shallow earthquakes in the depth range 0–30 km make up more than 60% of all world's
earthquakes. However, resolving their seismic source parameters such as the depth and …

Green functions (GFs) are an essential ingredient in waveform-based earthquake source
inversions. Hence, the error due to imprecise knowledge of a crustal velocity model is one of …

Despite advanced seismological techniques, automatic source characterization for
microseismic earthquakes remains difficult and challenging since current inversion and …