Seismic tomography is ubiquitously applied to image the structure of the Earth's mantle and crust on all scales. Dozens of tomographic models exist on...

The understanding of continental rift evolution in the absence of volcanism remains limited, as magmatic thermal weakening is critical for strain focu...

Signed amplitudes (amplitudes and polarities) of seismic body waves recorded by a single, three-component seismometer can constrain the strike, dip, a...

Many rifted margins and active continental rift systems host volcanic-rich and non-volcanic segments. While magma-assisted extension and the associate...

Long-lived GSN stations on the African continent are favorably positioned for recording SKS waves from tens to hundreds of well-distributed teleseismi...

Studies of Moho depth heterogeneity beneath the western branch of the East African Rift System (EARS) are limited to regions and localities where temp...

Seismic data in urban environments are dominated by man-made noise sources (e.g. traffic, construction, quarry blasts), which can falsely trigger eart...

Continental rifting is a critical component of the plate tectonics paradigm. We focus on advancing our understanding of magma-poor (dry) continental r...