Carbon from Earth's interior is thought to be released to the atmosphere mostly via
degassing of CO2 from active volcanoes,,,. CO2 can also escape along faults away from …

We use teleseismic waveform inversion, along with depth phase analysis, to constrain the
centroid depths and source parameters of large African earthquakes. The majority of seismic …

While the surface of Tibet is undergoing pervasive pure shear, stable terranes, straddling
subsurface sutures, remain in the sub-continental lithospheric mantle (SCLM), attesting to its …

Résumé The Mayotte seismic sequence that started on 10 May 2018, with a main shock of
magnitude Mw 5.9 on May 15, followed by a major offshore volcanic activity, raises several …

On the basis of a comprehensive data set of precisely determined depths of 121 large to
moderate‐sized earthquakes along and near the entire East African Rift System (EARS) …

Deep intracontinental earthquakes are poorly understood, despite their potential to cause
significant destruction. Although lower crustal strength is currently a topic of debate, dry …

This paper discusses the results of field-based geological investigations of exhumed rocks
exposed in the Musgrave Ranges (Central Australia) and in Nusfjord (Lofoten, Norway) that …

Although magmatism may occur during the earliest stages of continental rifting, its role in
strain accommodation remains weakly constrained by largely 2‐D studies. We analyze …

The rifting cycle initiates with stress buildup, release as earthquakes and/or magma
intrusions/eruptions, and visco-elastic rebound, multiple episodes of which combine to …

The well‐established variation in the depth of earthquakes along both branches of the East
African Rift System offers an opportunity to probe the controls on the depth‐extent of …