Overriding plate shortening and extension above subduction zones: A parametric study to explain formation of the Andes Mountains

Wouter P. Schellart*

*Corresponding author for this work

Research output: Contribution to JournalArticleAcademicpeer-review


Mountain building above subduction zones, such as observed in the Andes, is enigmatic, and the key parameter controlling the underlying dynamics remains a matter of considerable debate. A global survey of subduction zones is presented here, illustrating the correlation between overriding plate deformation rate and twelve physical parameters: overriding plate velocity, subducting plate velocity, trench velocity, convergence velocity, subduction velocity, subduction zone accretion rate, subducting plate age, subduction polarity, shallow slab dip, deep slab dip, lateral slab edge proximity, and subducting ridge proximity. All correlation coefficients are low ( R ≤ 0.39), irrespective of the global reference frame, relative plate motion model, or overriding plate deformation model, except for the trench velocity (0.33-0.68, exact value depends on adopted global reference frame) and subduction velocity, which shows an anticorrelation (0.55-0.57). This implies that no individual parameter can explain overriding plate deformation, except that trench retreat generally corresponds to extension while an approximately stable trench or trench advance generally corresponds to shortening. Understanding of the variety of strain patterns is obtained when slab edge proximity and overriding plate velocity are combined. Orogenesis occurs in overriding plates bordering central regions of wide subduction zones (≥∼4000 km) when the overriding plate is moving trenchward at 0-2 cm/yr (e.g., Andes, Japan). Because the center of a wide slab offers large resistance to lateral migration, the overriding plate effectively collides with the subduction hinge, forcing the slab to attain a shallow dip angle (e.g., Nazca and Japan slabs). Overriding plate extension is only found close to lateral slab edges or during overriding plate motion away from the center of a wide subduction zone, but in the latter scenario, maximum extension velocities are much lower than in the former scenario. For subduction settings close to lateral slab edges, overriding plate motion plays no significant role in overriding plate deformation. Thus, for rapid overriding plate extension, the key ingredient is rapid trench retreat, which only occurs close to lateral slab edges, while for overriding plate shortening, the key ingredients are (1) the resistance to rapid trench and hinge retreat, which occurs far from lateral slab edges, and (2) trenchward overriding plate motion.

Original languageEnglish
Pages (from-to)1441-1454
Number of pages14
JournalGeological Society of America Bulletin
Issue number11-12
Publication statusPublished - 2008


  • Andes
  • Deformation
  • Mountain building
  • Overriding plate
  • Slab
  • Subduction


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