The initial opening of the Africa-Antarctica Corridor, in the heart of Gondwana, is still
enigmatic due to missing information on the origin of major crustal features and the exact …

Several recent models of crustal evolution are based on the belief that the thickness of the
continental crust is proportional to its age, with ancient crust being the thickest. A worldwide …

The formation and disruption of supercontinents exert major influence on mantle dynamics
and have important bearing on continental dynamics and mineral systems. Here we …

The Limpopo Belt is a zone of thickened Archaean crust whose origin is currently explained
by a late Archaean continent-continent collision between the Kaapvaal and Zimbabwe …

Abstract Granulite metamorphism in the> 2.65 Ga Limpopo Belt of southern Africa is related
to crustal thickening, due to late Archaean collision tectonics. The Central Zone of the belt is …

The break-up of the Gondwana supercontinent resulted in the formation of the Central
Mozambique passive margin as Africa and Antarctica were separated during the mid …

The water saturation of a hydrocarbon bearing formation is usually calculated via the
conductivity of the formation water, as defined by Archie, 1942. However, in some formations …

Despite many years of work, a convincing evolutionary model for the Limpopo belt and its
geometrical relation to the surrounding cratons is still elusive. This is partly due to the …

Archaean cratons are the stable remnants of Earth's early continental lithosphere, and their
structure, composition and survival over geological time make them unique features of the …

A variety of structures results from the interplay of evolving far‐field forces, plate kinematics,
and magmatic activity during continental break‐up. The east Limpopo transform margin …