Role of subducted sediments in plate interface dynamics and forearc topography: Observations and modelling constraints for the Andes

COSENTINO, N. J.; CREMPIEN, J. G. F.; ARON, F. A.; MORGAN, J. P.; JORDAN, T. E.

Viena

Congreso; EGU 2019; 2019

EGU

Forearc topography and inferred paleotopography are key constraints on the processes acting at plate interfacesalong subduction margins. We used along-strike variations in modern topography, trench sediment thickness, andinstrumental seismic data sets over >2000 km of the Chilean margin to test previously proposed feedbacks amongsubducted sediments, plate interface rheology, megathrust seismicity, and forearc elevation. Observed correlationsare consistent with subducted sediments playing a prominent role in controlling plate interface rheology, which,in turn, controls the downdip distribution of megathrust seismicity and long-term forearc elevation.This control suggests that the Andean subduction plate interface (19.5-39.5ºS) constitutes a subductionchannel, able to accommodate long-term sediment flow in the downdip direction to depths greater than the updipend of the seismogenic zone. We explored numerically the role of subduction channel flow on forearc surfaceelevation. Results show that low (high) rates of trench sedimentation promote long-term interseismic coupledoffshore forearc subsidence (uplift) and onshore forearc platform uplift (subsidence), due to long-term viscoelasticflow in a strengthened (weakened) finite-thickness subduction channel. Low trench sedimentation rates may alsopromote deeper megathrust seismic slip, enhancing short-wavelength coastal zone uplift.The high elevation of the onshore forearc platform in northern Chile cannot be accounted for by previouslyproposed tectonic mechanisms such as coastal underplating and coseismic deformation, whose topographiceffects are restricted to the coastal zone. This section of the Andean forearc is particularly suited to test theabove-mentioned feedbacks, given that the extremely low denudation rates of this hyperarid region have allowedbetter reconstructions of the histories of paleo-elevations and paleoclimate compared to other sections of theforearc. These histories, together with modern data sets and numerical experiments, are consistent with the onsetof hyperaridity in the coastal zone at 25?20 Ma triggering (1) trench sediment starvation, (2) a rise in shear stressat the top of the subduction channel, (2) long-term, long-wavelength offshore forearc subsidence and onshoreforearc uplift, and (4) acceleration of short-wavelength coastal zone uplift.