Rifted margin architecture and crustal rheology: Reviewing Iberia-Newfoundland, Central South Atlantic, and South China Sea
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文摘
We review 3 magma-poor margins combining observations and numerical modelling. We describe three characteristic phases: (1) simultaneous faulting, (2) rift migration, and (3) break-up. Weak rheologies prolong the phase of simultaneous faulting. The rift migration phase is enabled by initial fault asymmetry and weak crust.

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