Abstract The Cenozoic East African rift (EAR), Cameroon Volcanic Line (CVL), and Atlas
Mountains formed on the slow‐moving African continent, which last experienced orogeny …

This paper presents a new model of the shear velocity structure of the crust and uppermost
mantle beneath the contiguous US The model is based on more than a decade of USArray …

We present a novel method for joint inversion of receiver functions and surface wave
dispersion data, using a transdimensional Bayesian formulation. This class of algorithm …

Explaining the cause and support of Africa's varied topography remains a fundamental
question for our understanding of the long-term evolution of the continent. As geodynamical …

A non-linear Bayesian Monte-Carlo method is presented to estimate a Vsv model beneath
stations by jointly interpreting Rayleigh wave dispersion and receiver functions and …

Rayleigh wave phase velocity maps from ambient noise and earthquake data are inverted
jointly with receiver functions observed at 828 stations from the USArray Transportable Array …

Our understanding of the tectonic development of the African continent and the interplay
between its geological provinces is hindered by unevenly distributed seismic …

Intra-and trans-continental tectonic lineaments and tectonic structures cutting Africa and
Gondwana have long been identified by many authors. These structures were initially …

We present new crust and lithosphere thickness maps of the African mainland based on
integrated modeling of elevation and geoid data and thermal analysis. The approach …

The origin of the Cameroon Volcanic Line (CVL), a 1600 km long linear volcanic chain
without age progression that crosses the ocean‐continent boundary in west‐central Africa, is …