The Pacific Ocean formed through Neoproterozoic rifting of Rodinia and despite a long
history of plate convergence, this ocean has never subsequently closed. The record of …

Age relations for assembly of Gondwana and Pangea indicate that the timing of collisional
orogenesis between amalgamating continental bodies was synchronous with subduction …

In the last 1000 million years, Australia has been part of two supercontinents: Palaeozoic
Gondwanaland and Neoproterozoic Rodinia. Neoproterozoic Australia was covered by …

Abstract The Tasmanides of eastern Australia record the break-up of Rodinia, followed by
the growth of orogenic belts along the eastern margin of Gondwana. Spatially, the …

Tectonically, the Sanjiang Tethyan Metallogenic Domain (STMD) is located within the
eastern Himalayan–Tibetan Orogen in the Sanjiang Tethys, southwestern China. Although …

Abstract The Antarctic Ross and the Australian Delamerian orogenies are the consequence
of stress transfer to the outboard trailing edge of the newly assembled Gondwana …

The Tasmanides occupy the eastern third of Australia and provide an extensive record of the
evolution of the eastern Gondwanan convergent plate boundary from the Cambrian to the …

The explosive radiation of animals on Earth during the late Early Cambrian period (∼ 530–
510 Ma) coincides with the deposition of enormous volumes of continentally derived …

The well-known southwest-to-northeast younging of stratigraphy over a present-day cross
strike distance of> 1500 km in the southern Tasmanides of eastern Australia has been used …

A review of U–Pb age data from intrusive and volcanic rocks for Antarctica and Australia has
highlighted the remarkable synchronicity in the shift from passive margin or continental arc …