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Strong Plate Coupling Along the Nazca–South America Convergent Margin

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Strong Plate Coupling Along the Nazca–South America Convergent Margin Strong plate coupling along the Nazca–South America convergent margin Giampiero Iaffaldano* Geophysics Section, Department of Earth and Environmental Sciences, Ludwig-Maximilians University, Hans-Peter Bunge Munich 80333, Germany ABSTRACT complexity of the dynamic system by exploiting The force balance in plate tectonics is fundamentally important but poorly known. Here, isostasy and vertical integration of stresses in the we show that two prominent and seemingly unrelated observations—trench-parallel gravity so-called thin-shell approximation, although a anomalies along the Nazca–South America margin that coincide with the rupture zones of shortcoming arises from the need to parameter- great earthquakes, and a rapid slowdown of Nazca–South America convergence over the past ize the mantle buoyancy and fl ow that generate 10 m.y.—provide key insights. Both result from rapid Miocene-Pliocene uplift of the Andes shear stresses at the base of plates. At the same and provide quantitative measures of the magnitude and distribution of plate coupling along time, there has been great progress in our abil- the Nazca–South America margin. We compute the plate-tectonic force budget using global ity to simulate the circulation of Earth’s mantle models of the faulted lithosphere coupled to high-resolution mantle circulation models and at high numerical resolution (Bunge et al., 1997). fi nd that Andean-related plate-margin forces are comparable to plate-driving forces from the Such time-dependent Earth models account for mantle, and they have suffi cient magnitude to account for pronounced bathymetry variations radial variations in mantle viscosity (typically a along the trench. Our results suggest that plate coupling, gravity anomalies, and bathymetry factor 40 increase from the upper to the lower variations along a given trench are all controlled by long-term stress variations in the upper mantle), internal heat generation from radioactiv- portion of plate boundaries and that an explicit budget of driving and resisting forces in plate ity, bottom heating from the core, and a history tectonics can be obtained. For the convergent margin considered here, spatial variations in of subduction spanning the past 120 m.y., and the effective coeffi cient of friction associated with the distribution of lubricating sediments they provide a fi rst-order estimate of the internal entering the trench are, by comparison, of minor importance. mantle buoyancy forces that drive the plates; the models, however, do not account for the brittle Keywords: Andean uplift, plate coupling, gravity anomalies. nature of the faulted lithosphere and, specifi cally, for the contribution of plate-boundary forces INTRODUCTION anomalies (Fig. 2A). We computed these anom- to the stress balance. It is logical therefore to Plate tectonics (Morgan, 1968) is remark- alies by subtracting the regional-average trench- merge these two independent classes of models. able in that they explain the surface motion normal gravity profi le from free-air gravity data Using the global model for lithosphere dynamics of Earth with great accuracy (DeMets et al., (Sandwell and Smith, 1997). The trench-parallel SHELLS (Kong and Bird, 1995) combined with 1994), even though the budget of driving and gravity anomaly profi le along the Nazca–South three-dimensional (3-D) mantle circulation mod- resisting forces is poorly known (Forsyth and America margin is characterized by strongly els (Bunge et al., 2002), we have shown recently Uyeda, 1975). Mantle convection is commonly negative values, as large as −100 mGal, in the that late Miocene-Pliocene uplift of the Andes accepted as the engine for plate motion (Ricard central part close to the highly elevated Puna can account for the rapid Nazca–South America and Vigny, 1989), but the magnitude and distri- and Altiplano regions. In contrast, the northern convergence reduction over the past 10 m.y. bution of resisting plate-margin forces are less and southern parts of the trench both show a (Iaffaldano et al., 2006). clear. Short-term plate-motion changes on the positive signal. Trench-parallel gravity anomaly order of a few million years or less, which are gradients coincide with the occurrence of large MODELS AND RESULTS increasingly revealed through the comparison earthquakes—such as the great M 9.5 Chilean Global coupled lithosphere-mantle circulation of geodesy-based measurements (Dixon, 1991; event of 1960 (Barrientos and Ward, 1990) and models allow us to derive an explicit budget of Stein, 1993) and increasingly detailed paleomag- the recent M 8.0 Peru earthquake of 2007— plate-boundary forces along the Nazca–South netic reconstructions (Müller et al., 2008), repre- and are associated with substantial trench- America plate margin. Under the assumption sent a powerful probe to quantify these forces. parallel bathymetry variations (Smith and that plate-boundary forces along the margin are Since rapid plate-velocity variations are unlikely Sandwell, 1997). It has been suggested that the dominated by the recent uplift of the Andes, we to result from changes in the pattern of global largest earthquakes occur on portions of sub- used the SHELLS global model, which accounts mantle fl ow, which evolves on a much longer duction zones where plates are most strongly for the present-day topography as reported in the time scale, on the order of 150–200 m.y. (Bunge coupled (Kanamori, 1986); thus, trench-parallel ETOPO5 data set (National Geophysical Data et al., 1998), they must refl ect temporal varia- gravity anomalies might be indicative of lateral Center, 1998), and shear tractions taken from tions in plate coupling along a given margin. A variations in mechanical coupling (Stein and the aforementioned simulations of mantle fl ow prominent example is the 30% slowing of con- Wysession, 2003) along the plate margin. to compute equilibrium forces in the lithosphere. vergence between the Nazca and South America One way to estimate plate coupling is from We then performed a second simulation corre- plates over the past 10 m.y. (Fig. 1) inferred from computer simulations using global models of sponding to a paleoreconstruction of topography a variety of data (Norabuena et al., 1999). the lithosphere that include sophisticated rheol- of the Andes 10 m.y. ago (Gregory-Wodzicki , We propose that the slowing of convergence ogies and realistic plate confi gurations (Bird, 2000). The plate-boundary forces along the results from the same mechanism that causes 1999). The stresses involved in the dynamics Nazca–South America margin that correspond pronounced along-strike trench-parallel gravity of the lithosphere include the tectonic contribu- to the recent uplift of the Andes were obtained tion coming from regions of high topography, as the difference of the two simulations. It is which provide both horizontal deviatoric stresses worth mentioning that among others, one advan- *Current address: Department of Earth and Plan- etary Sciences, Harvard University, Cambridge, and vertical overburden pressure, and the shear tage of such an approach is that it allows us to Massachusetts 02138, USA: E-mail: iaffaldano@ stresses from buoyancies in the mantle. Typi- neglect, with reasonable confi dence, viscous eps.harvard.edu. cally, these models reduce the computational deformation within the Andean belt, since its © 2008 The Geological Society of America. For permission to copy, contact Copyright Permissions, GSA, or [email protected]. GEOLOGY,Geology, June June 2008; 2008 v. 36; no. 6; p. 443–446; doi: 10.1130/G24489A.1; 4 fi gures. 443 for the associated mass anomalies. Our predicted trench-parallel resisting force anomalies display a similar behavior. Gravity and resisting force anomalies along the trench are highly correlated at the 90% confi dence level (Fig. 2C). In Figure 3A, we plot the observed trench- parallel bathymetry anomalies obtained by subtracting the average trench-parallel bathy- metric profi le from the digital elevation model ETOPO5. The trench-parallel gravity (Fig. 2A) and bathymetry (Fig. 3A) anomalies are in excellent agreement, an inference suggested earlier by Song and Simons (2003): negative gravity anomalies correspond to deeper-than- average bathymetry, whereas positive anomalies correspond to bathymetry that is shallower than the average. We note that the age of the Nazca ocean fl oor varies between 20 and 50 m.y. old along the margin (Müller et al., 1997), and that a simple half-space model of plate subsidence due to lithosphere cooling would predict ocean depth variation of ~1 km, accounting for only 25% of the observed bathymetric variations. Figure 1. Comparison of past (10 m.y.; red) and present-day (blue) motion of Nazca (NZ) and We tested whether the magnitude of plate- South America (SA), derived from paleomagnetic (red) and instantaneous geodetic observa- coupling forces arising from our simulations was tions (blue). Velocity vectors reveal a 30% convergence reduction from 10 to 7 cm/yr over the suffi cient to explain the observed bathymetry past 10 m.y. Timing suggests a co-evolution of increased plate-coupling forces and Andean signal by solving for an analytical solution of the uplift. Plate boundaries are in black; continents are in gray. Plate abbreviations: AF—Africa, AN—Antarctica, CA—Caribbean, CO—Cocos, PA—Pacifi c. thin-plate differential equation for a semi-infi nite oceanic plate, tectonically loaded on one side (see inset in Fig. 3B). We assumed a Young’s modulus growth is included in our simulations not as a as the trench-parallel gravity
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