1. Geological Sciences and Geological Engineering, Queen's University, Kingston, Ontario K7L 3N6, Canada
2. School of Biology, Earth and Environmental Sciences, University of New South Wales, Sydney, New South Wales 2052, Australia
3. Géosciences Rennes, CNRS UMR 6118, Université de Rennes 1, Rennes F-35042, France

Correspondence to: James K. W. Lee¹ Correspondence and requests for materials should be addressed to J.K.W.L. (Email: lee@geol.queensu.ca).

Abstract

Collision tectonics and the associated transformation of continental crust to high-pressure rocks (eclogites) are generally well-understood processes, but important contradictions remain between tectonothermal models and petrological–isotopic data obtained from such rocks. Here we use ⁴⁰Ar–³⁹Ar data coupled with a thermal model to constrain the time-integrated duration of an orogenic cycle (the burial and exhumation of a particular segment of the crust) to be less than 13 Myr. We also determine the total duration of associated metamorphic events to be 20 kyr, and of individual heat pulses experienced by the rocks to be as short as 10 years. Such short timescales are indicative of rapid tectonic processes associated with catastrophic deformation events (earthquakes). Such events triggered transient heat advection by hot fluid along deformation (shear) zones, which cut relatively cool and dry subducted crust. In contrast to current thermal models that assume thermal equilibrium and invoke high ambient temperatures in the thickened crust, our non-steady-state cold-crust model satisfactorily explains several otherwise contradictory geological observations.

1. Geological Sciences and Geological Engineering, Queen's University, Kingston, Ontario K7L 3N6, Canada
2. School of Biology, Earth and Environmental Sciences, University of New South Wales, Sydney, New South Wales 2052, Australia
3. Géosciences Rennes, CNRS UMR 6118, Université de Rennes 1, Rennes F-35042, France

Correspondence to: James K. W. Lee¹ Correspondence and requests for materials should be addressed to J.K.W.L. (Email: lee@geol.queensu.ca).

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