Megathrust shear force controls mountain height at convergent plate margins

Author:

Dielforder ArminORCID,Hetzel Ralf,Oncken Onno

Publisher

Springer Science and Business Media LLC

Subject

Multidisciplinary

Reference78 articles.

1. Husson, L. & Ricard, Y. Stress balance above subduction: application to the Andes. Earth Planet. Sci. Lett. 222, 1037–1050 (2004).

2. Wang, K. & He, J. Mechanics of low-stress forearcs: Nankai and Cascadia. J. Geophys. Res. 104, 15191–15205 (1999).

3. Lamb, S. Shear stresses on megathrusts: implications for mountain building behind subduction zones. J. Geophys. Res. 111, B07401 (2006).

4. Lamb, S. & Davis, P. Cenozoic climate change as a possible cause for the rise of the Andes. Nature 425, 792–797 (2003).

5. Champagnac, J. D., Molnar, P., Sue, C. & Herman, F. Tectonics, climate, and mountain topography. J. Geophys. Res. 117, B02403 (2012).

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