Abstract The Sorgenfrei-Tornquist Zone (STZ) is the northwestern segment of the Tornquist
Zone and extends from Bornholm across the Baltic Sea and northern Denmark into the North …

The 3D geometrical evolution of the Barents Sea Ice Sheet (BSIS), particularly during its late-
glacial retreat phase, remains largely ambiguous due to the paucity of direct marine-and …

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 Gravity field and steady-state Ocean Circulation Explorer (GOCE) satellite aimed at
determining the Earth's mean gravity field. GOCE delivered gravity gradients containing …

We investigate the lithospheric structure of the Iberian Peninsula and lateral crustal density
variations using a three-step approach. First the crustal and mantle lithosphere thicknesses …

The crust–mantle boundary (the Moho) is a first order interface in the Earth and the depth to
the Moho is therefore well studied in most regions. However, below regions which are …

The long-wavelength gravity field contains information about processes in the
sublithospheric mantle. As satellite-derived gravity models now provide the long to medium …

A review of the early Holocene paleoseismicity in areas covered by huge ice sheets in the
interior of Fennoscandia and North America shows that observational data and numerical …

The Antarctic ice sheet (AIS) lies on a solid Earth that displays large spatial variations in
rheological properties, with a thin lithosphere and low‐viscosity upper mantle (weak Earth …

The aim of this paper is to present the concept of a dedicated gravity field mission for the
planet Mars, the Mars Quantum Gravity Mission (MaQuIs). The mission is targeted at …