Letter | Published:

The role of crustal quartz in controlling Cordilleran deformation

Nature volume 471, pages 353357 (17 March 2011) | Download Citation

Abstract

Large-scale deformation of continents remains poorly understood more than 40 years after the plate tectonic revolution1. Rock flow strength and mass density variations both contribute to stress, so both are certain to be important, but these depend (somewhat nebulously) on rock type, temperature and whether or not unbound water is present2. Hence, it is unclear precisely how Earth material properties translate to continental deformation zones ranging from tens to thousands of kilometres in width, why deforming zones are sometimes interspersed with non-deforming blocks and why large earthquakes occasionally rupture in otherwise stable continental interiors. An important clue comes from observations that mountain belts and rift zones cyclically form at the same locations despite separation across vast gulfs of time3 (dubbed the Wilson tectonic cycle), accompanied by inversion of extensional basins4 and reactivation of faults and other structures formed in previous deformation events5. Here we show that the abundance of crustal quartz, the weakest mineral in continental rocks2, may strongly condition continental temperature and deformation. We use EarthScope seismic receiver functions6, gravity and surface heat flow measurements7 to estimate thickness and seismic velocity ratio, vP/vS, of continental crust in the western United States. The ratio vP/vS is relatively insensitive to temperature but very sensitive to quartz abundance8,9. Our results demonstrate a surprising correlation of low crustal vP/vS with both higher lithospheric temperature and deformation of the Cordillera, the mountainous region of the western United States. The most plausible explanation for the relationship to temperature is a robust dynamical feedback, in which ductile strain first localizes in relatively weak, quartz-rich crust, and then initiates processes that promote advective warming, hydration and further weakening. The feedback mechanism proposed here would not only explain stationarity and spatial distributions of deformation, but also lend insight into the timing and distribution of thermal uplift10 and observations of deep-derived fluids in springs11.

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Acknowledgements

We thank K. Dueker, G. Pavlis, T. Ravat, J. Shervais and D. Schutt for discussions, and A. Braathen and R. Bürgmann for comments. We are grateful to P. Crotwell, T. Owens and members of IRIS for their efforts on the EARS database, and to P. Crotwell and B. Kucks for help with data acquisition. The work of A.R.L. on this project was supported by National Science Foundation grants EAR-0454541 (EarthScope Science: Rio Grande Rift) and EAR-0955909 (Geophysics/EarthScope CAREER: Deformation Processes), and by a Utah State University New Faculty Research Grant.

Author information

Affiliations

  1. Department of Geology, Utah State University, Logan, Utah 84322-4505, USA

    • Anthony R. Lowry
  2. Department of Earth Sciences, Royal Holloway, University of London, Egham, Surrey TW20 0EX, UK

    • Marta Pérez-Gussinyé

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Contributions

A.R.L. developed and implemented the joint receiver function/gravity/heatflow inversion for crustal thickness and vP/vS. M.P.-G. developed and implemented the inversion for effective elastic thickness. The manuscript was written by A.R.L with contributions from M.P.-G.

Competing interests

The authors declare no competing financial interests.

Corresponding author

Correspondence to Anthony R. Lowry.

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https://doi.org/10.1038/nature09912

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