West Antarctica has formed the tectonically active margin between East Antarctica and the
Pacific Ocean for almost half a billion years, where it has recorded a dynamic history of …

The latest seismic data and improved information about the subglacial bedrock relief are
used in this study to estimate the sediment and crustal thickness under the Antarctic …

The Mesozoic opening history of the Southern Ocean between South America, Africa, and
Antarctica is one of the largest gaps in knowledge on the evolution of this region. Competing …

In this paper, we review the dimensions, geometry and architecture of the components of the
Kalahari Craton and the various positions this important crustal block could have occupied …

Heimefrontfjella in western Dronning Maud Land, East Antarctica, is part of the c. 1.1 Ga
Namaqua–Natal–Maud Belt. It is situated at an important location, both for Rodinia …

Gondwana breakup changed the global continental configuration, leading to opening of
major oceanic gateways, shifts in the climate system and significant impacts on the …

Abstract The Grunehogna Craton (GC, East Antarctica) is interpreted as part of the Archaean
Kaapvaal Craton of southern Africa prior to Gondwana breakup. The basement of the GC is …

A new method for modeling heat flux shows that the upper crust contributes up to 70% of the
Antarctic Peninsula's subglacial heat flux and that heat flux values are more variable at …

New SHRIMP zircon data from Gjelsvikfjella and Mühlig–Hofmann–Gebirge (East
Antarctica) indicate that the metamorphic basement is composed of Grenville-age rocks that …

The Sør Rondane Mountains (SRM) in eastern Dronning Maud Land (DML) are located in
an area, where two apparent Pan-African (650–520 Ma) orogenic mobile belts appear to …