The role of megacontinents in the supercontinent cycle

Paleomagnetic constraints on the duration of the Australia-Laurentia connection in the core of the Nuna supercontinent

Secular isotopic variation in lithospheric mantle through the Variscan orogen: Neoproterozoic to Cenozoic magmatism in continental Europe

How was the Iapetus Ocean infected with subduction?

Whither the supercontinent cycle?

Provenance and tectonic evolution of Ganderia: Constraints on the evolution of the Iapetus and Rheic oceans

Lithospheric delamination in the core of Pangea: Sm-Nd insights from the Iberian mantle

Supercontinent reconstruction from recognition of leading continental edges

The Pangea conundrum

Continental mafic magmatism of different ages in the same terrane: Constraints on the evolution of an enriched mantle source

Acatlán Complex, southern Mexico: Record spanning the assembly and breakup of Pangea

Origin of the Rheic Ocean: Rifting along a Neoproterozoic suture?

Contiguous rather than discrete Paleozoic histories for the Avalon and Meguma terranes based on detrital zircon data

Do supercontinents introvert or extrovert?: Sm-Nd isotope evidence

Middle to late Paleozoic Acadian orogeny in the northern Appalachians: A Laramide-style plume-modified orogeny?

Plume-modified orogeny: An example from the western United States

Is the ancestral Yellowstone hotspot responsible for the Tertiary “Carlin” mineralization in the Great Basin of Nevada?

Contrasting basement isotopic signatures and the palinspastic restoration of peripheral orogens: Example from the Neoproterozoic Avalonian-Cadomian belt

Supercontinent model for the contrasting character of Late Proterozoic orogenic belts

Tectonic control on the origin and orientation of igneous layering: An example from the Greendale Complex,Antigonish Highlands, Nova Scotia, Canada