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Earth science

Palaeo-altimetry of Tibet (reply)

Naturevolume 444pagesE4E5 (2006) | Download Citation

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Abstract

Molnar et al.1 question our conclusion on the role of convective destabilization of thickened mantle lithosphere in determining the surface elevation history of the Tibetan plateau. The primary argument depends on our interpretation2,3 of oxygen-isotope-based estimates of palaeo-elevation of the Lunpola basin, a locality in the centre of the plateau.

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References

  1. 1

    Molnar, P., Houseman, G. A. & England, P. C. Nature 444, doi:10.1038/nature05368 (2006).

  2. 2

    Rowley, D. B. & Currie, B. S. Nature 439, 677–681 (2006).

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    Rowley, D. B., Pierrehumbert, R. T. & Currie, B. S. Earth Planet. Sci. Lett. 188, 253–268 (2001).

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    Molnar, P., England, P. & Martinod, J. Rev. Geophys. 31, 357–396 (1993).

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    Kapp, P., Yin, A., Harrison, T. M. & Ding, L. Geol. Soc. Am. Bull. 117, 865–878 (2005).

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    Pysklywec, R. N., Beaumont, C. & Fullsack, P. Geology 28, 655–658 (2000).

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Affiliations

  1. Department of Geophysical Sciences, University of Chicago, Chicago, 60637, Illinois, USA

    • D. B. Rowley
  2. Department of Geology, Miami University, Oxford, Ohio, 45056, USA

    • B. S. Currie

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Correspondence to D. B. Rowley.

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https://doi.org/10.1038/nature05369

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