The subduction zone at the western margin of South America is the living paradigm for the A-type (or Chilean-type) of subduction, which is the geodynamic system that appears to have generated the largest earthquakes and tsunamis, as well as one of the largest mountain belt - and high-plateau- systems of our planet; the Andes. At the subduction interface, there is a fundamental partitioning between mechanisms leading to these two processes. It is now clear (contrary to expectations ascribed to C. Darwin) that crustal deformation associated with any large subduction earthquake on Earth leaves no significant contribution to mountain building. The alternative idea attributing the Andean orogenic growth to large-scale accretion of intrusive bodies and volcanism is in conflict with the tectonic shortening mechanisms now admitted for explaining the orogenic relief in collision belts (Alps, Himalayas). Simply, no first-order unified theory is available for present-day orogeny occurring in our planet.
The growth of the Andean orogen by tectonic shortening (associated with plate convergence) can now be measured over the 103-107 yr time scale, which is barely longer than the seismic cycle observed for subduction earthquakes. However, how those two fundamental processes interact is unknown and no current geodynamic model appears to explain satisfactorily both, the generation of the large earthquakes and the topographic relief generated (by some combination of accretion and tectonic shortening) as an end product of the same subduction system.
Our main objectives concerns :
- Plate coupling processes that eventually resume in megathrust earthquake ruptures; including tectonic complexities, at and near the plate interface, which drive segmentation.
- Geometry and kinematics of faulting at the Western Andean front; past earthquake ruptures and associated seismic hazards.
- Large-scale tectonic evolution and geodynamics of the Andean orogeny coupled with Caenozoic global climate changes.
Learn more on Robin Lacassin web page about Andean Orogeny