Articles | Volume 9, issue 3
Solid Earth, 9, 599–627, 2018
https://doi.org/10.5194/se-9-599-2018
Solid Earth, 9, 599–627, 2018
https://doi.org/10.5194/se-9-599-2018
Research article
08 May 2018
Research article | 08 May 2018

Testing the effects of topography, geometry, and kinematics on modeled thermochronometer cooling ages in the eastern Bhutan Himalaya

Michelle E. Gilmore et al.

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Cited articles

Adams, B. A., Hodges, K. V., van Soest, M. C., and Whipple, K. X.: Evidence for Pliocene-Quaternary normal faulting in the hinterland of the Bhutan Himalaya, Lithosphere, 5, 438–449, https://doi.org/10.1130/l277.1, 2013.
Adams, B. A., Whipple, K. X., Hodges, K. V., and Heimsath, A. M.: In situ development of high-elevation, low-relief landscapes via duplex deformation in the Eastern Himalayan hinterland, Bhutan, J. Geophys. Res.-Earth, 121, 294–319, https://doi.org/10.1002/2015JF003508, 2016.
Adlakha, V. A., Lang, K. A., Patel, R. C., Lal, N., and Huntington, K. W.: Rapid long-term erosion in the rain shadow of the Shillong Plateau, Eastern Himalaya, Tectonophysics, 582, 76–83, https://doi.org/10.1016/j.tecto.2012.09.022, 2013.
Almendral, A., Robles, W., Parra, M., Mora, A., and Ketcham, R.: FetKin: Coupling kinematic restorations and temperature to predict thrusting, exhumation histories, and thermochronometric ages, AAPG Bulletin, 99, 1557–1573, https://doi.org/10.1306/07071411112, 2015.
Avouac, J.-P.: Dynamic processes in extensional and compressional settings–Mountain building: From earthquakes to geological deformation, in: Crust and Lithosphere Dynamics, Treatise on Geophysics, 6, edited by: Schubert, G. and Watts, A. B., Elsevier, Boston, 377–439, https://doi.org/10.1016/B978-044452748-6.00112-7, 2007.
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Short summary
We examine the Himalayan Mountains of Bhutan by integrating balanced geologic cross sections with cooling ages from a suite of mineral systems. Interpretations of cooling ages are intrinsically linked to both the motion along faults as well as the location and magnitude of erosion. In this study, we use flexural and thermal kinematic models to understand the sensitivity of predicted cooling ages to changes in fault kinematics, geometry, and topography.