The relationship between plate curvature and elastic plate thickness : a study of the Peru-Chile Trench
The relationship between plate curvature and elastic plate thickness : a study of the Peru-Chile Trench
Date
1988-05
Authors
Judge, Anne Victoria
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Location
Peru-Chile Trench
DOI
10.1575/1912/4294
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Keywords
Plate tectonics
Abstract
The age of the Nazca plate where it enters the Peru and northern Chile trenches varies
from 30 Ma in the north to 45 Ma in the south as its dip beneath the South American
continent steepens from 13° to 30°. If the elastic thickness Te of oceanic lithosphere
depends only on its age, and therefore thermal state, we would expect that Te determined
from fitting the flexure of the lithosphere over the outer rise as revealed in the depth and
geoid anomalies would increase from the Peru Trench in the north to the northern Chile
Trench further south. We find that just the opposite is true: the lithosphere appears stiffer
outboard of the Peru Trench than it does further south, and the isotherm controlling the
elastic/ductile transition must be 600°C or greater if the thermal structure of the plate is that
predicted by the standard thermal plate model. Because the decrease in plate stiffness to the
south is correlated with a decrease in the minimum radius of curvature of the flexed plate
over the outer rise and outer trench wall, we interpret our result in terms of inelastic
yielding of the oceanic lithosphere when bent to high strains. The fact that the more highly
bent segment of subducting lithosphere also dips at a steeper angle at greater depth beneath
the continent might suggest that the amount of inelastic weakening of the lithosphere could
be predicted from seismic images of the down going slab, but we find little support for this
correlation worldwide. The forces and moments controlling the shallow deformation of the
plate seaward of the trench do not appear to be linked to upper mantle processes which
impose the dip at greater depth. Finally, we consider the possibility that the elastic
thickness of the lithosphere would be reduced for trenches that are highly arcuate in map
view, again due to inelastic yielding. If such a relationship exists, the effect for oceanic
lithosphere is much smaller than what is documented for continental plates where they
underthrust highly arcuate fold belts.
Description
Submitted in partial fulfillment of the requirements for the degree of Master of Science at the Massachusetts Institute of Technology and the Woods Hole Oceanographic Institution May 1988
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Citation
Judge, A. V. (1988). The relationship between plate curvature and elastic plate thickness : a study of the Peru-Chile Trench [Doctoral thesis, Massachusetts Institute of Technology and Woods Hole Oceanographic Institution]. Woods Hole Open Access Server. https://doi.org/10.1575/1912/4294