Permo-Triassic rift nucleation in East Antarctica revealed by low-temperature thermochronology
Researchers collected new apatite fission-track and (U-Th)/He data across more than 5000 km of the East Antarctic margin to reconstruct its rifting history. The results show that an earlier, failed rifting episode in the Permo-Triassic period cooled and shaped the crust more strongly than the later Jurassic-Cretaceous breakup of Gondwana itself. This multi-phase rifting appears … Read more…