MODERN-STYLE METAMORPHISM IN THE PALEOPROTEROZOIC: A PRODUCT OF STOCHASTICITY IN ‘TIME TO SUBDUCTION INITIATION’ WITHIN OCEAN BASINS? (Invited Presentation)
The life span of an ocean basin is not deterministic: compare Tuzo Wilson’s ‘Proto-Atlantic’ (the Iapetus Ocean), which underwent subduction initiation after 40–50 Myr, to the subsequent Atlantic Ocean, which has not seen subduction initiation in its >170 Myr history. Stochasticity in ‘time to subduction initiation’ within ocean basins affects the age and density of downgoing oceanic lithosphere and must thereby influence subduction zone geodynamics (i.e., hinge advance v. retreat and stress history of the overriding plate; e.g., East Pacific- v. West Pacific-style convergence). Stochasticity in the ‘survival time’ of tectonic elements may sometimes cause local tectonic responses that are atypical of a prevailing ‘stage’ in secular cooling, superimposing ‘randomness’ on a more general, monotonic tectonic evolution trend. Modern-style metamorphism at 2100–1750 Ma may record the development of exceptionally dense lithosphere within exceptionally old ocean basins, giving rise to geodynamic settings in the Paleoproterozoic that are more representative of the colder Phanerozoic than the earlier Earth.