The detection of a seismic boundary, the “Moho”, between the outermost shell of the Earth,
the Earth's crust, and the Earth's mantle by A. Mohorovičić was the consequence of …

Receiver functions for numerous teleseismic earthquakes recorded at 23 broadband and
mid-band stations in Saudi Arabia and Jordan were analyzed to map crustal thickness within …

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 …

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) …

Southern Africa, here taken as the region that comprises the Kalahari and southern Congo
Cratons, and the important orogenic belts that surrounded or separated them during the …

New estimates of crustal thickness, Poisson's ratio and crustal shear wave velocity have
been obtained for 39 stations in Angola, Botswana, the Democratic Republic of Congo …

Ambient noise autocorrelations can be used to reconstruct the seismic reflection response of
the Earth structure beneath single stations using continuous recordings without the need for …

We estimated the velocity structure beneath four three-component broad-band seismic
stations in the Sumatra region by the joint inversion of teleseismic receiver functions and …

The converted wave data (P-to-s or S-to-p), traditionally termed as receiver functions, are
often contaminated with noise of different origin that may lead to the erroneous identification …

We describe a waveform modelling technique and demonstrate its application to determine
the crust-and upper-mantle velocity structure beneath Africa. Our technique uses a …