Abstract The Transantarctic Mountains (TAM) are one of Earth's great mountain belts and
are a fundamental physiographic feature of Antarctica. They are continental-scale, traverse a …

During the period from the Neoproterozoic to the early Paleozoic, numerous continental
fragments in the Southern Hemisphere consolidated along a series of interconnected …

Ca. 415–400 Ma ultrahigh-pressure (UHP) eclogites in the Western Gneiss Region of
Norway occur in three discrete∼ 2500 km 2 to> 100 km 2 antiformal domains separated by …

We present the results of field investigations carried out at the southern termination of the
Priestley Fault, a major Cenozoic right-lateral strike-slip fault system in northern Victoria …

Cumulative, polymodal normal (Gaussian distribution) statistics was applied to subsidiary
fault data collected from damage zones associated with the Cenozoic Lanterman and …

Two major thrust systems with contrasting senses of displacement transect the Wilson
terrane crust of northern Victoria Land, Antarctica. Along both mylonitic shear zones the …

Relict granulite facies rocks of the region between Priestley and Aviator Glaciers (Wilson
Terrane, Ross Orogen) comprise an older supracrustal sequence which has been intruded …

The Lanterman Fault is one of the subvertical, NW–SE-striking intraplate shear zones that
bound the major Proterozoic to Early Palaeozoic tectono-metamorphic blocks constituting …

Granulite-facies rocks occur as mappable relics in the Wilson Terrane (northern Victoria
Land), the lithotectonic unit of the Cambro—Ordovician Ross orogen closest to the East …

The Terra Nova Intrusive Complex (TNIC) in northern Victoria Land, Antarctica, results from
widespread magmatism during the Early Paleozoic Ross Orogeny. According to field …