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Gondwanan continental collision drives gravitational spreading and collapse of the ancestral East Antarctic mountains Earth and Planetary Science Letters, 2025 (Ref: 17346)
Category 1: Peer-reviewed literature

Continent-continent collisions develop mature orogenic systems over tens of millions of years, creating a thermally weakened mid-crustal infrastructure layer (15–50 km deep) that flows laterally from the thickened mountain ranges or plateaus.

Macquarie Island's Finch-Langdon Fault Zone: A ridge-transform corner structure preserved along the pacific-Australian plate boundary Geological Society of America Abstracts with Programs, 2000 (Ref: 9367)
Category 3: Abstract

Macquarie Island, located along the Australian-Pacific transform plate boundary~1200 km south of New Zealand, consists of uplifted oceanic crust that still lies within the ocean basin where it formed. A lower crustal and upper mantle section of sheeted dikes…

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