Over the past decades, significant efforts have been made to understand the nature,
dynamics and evolution of volcanic systems. In parallel, the continuous demographic …

This chapter reviews glacial isostatic adjustment (GIA) and post-seismic deformation in
Antarctica. It discusses numerical models and their inputs, and observations and inferences …

The deployment of seismic stations and the development of ambient noise tomography as
well as new analysis methods provide an opportunity for higher-resolution imaging of …

We present a new magnetic compilation for Central Gondwana conformed to a recent
satellite magnetic model (LCS-1) with the help of an equivalent layer approach, resulting in …

This chapter reviews the geochemistry and petrology of mantle peridotite xenoliths from
across Antarctica, including parameters that are of most relevance to geophysical studies …

This chapter describes the application and coverage of gravity and magnetic data for
Antarctica with emphasis on airborne and satellite models. Low resolution satellite data help …

The Antarctic mantle, bounded between the core and the Mohorovičić discontinuity, is one of
the most difficult targets of study on Earth because of ice cover and rare outcrops. A …

Antarctic geothermal heat flux is a basic input variable for ice sheet dynamics simulation. It
greatly affects the temperature and mechanical properties at the bottom of the ice sheet …

High‐quality maps of Geothermal heat flow (GHF) are crucial when modeling ice dynamics,
shape, and mass loss of the Antarctic Ice Sheet, which is one of the largest potential …

The thermal state of the lithosphere and related geothermal heat flow (GHF) is a crucial
parameter to understand a variety of processes related to cryospheric, geospheric, and/or …