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An analytical solution for the exhumation of an orogenic wedge and a comparison with thermochronology data
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Abstract
Thermochronology data is key for quantifying the exhumation history and dynamics of mountain belts. Here we present a new analytical solution for the steady-state exhumation of an orogenic wedge that undergoes transport along a basal detachment, uniform internal deformation, basal and frontal accretion. The solution predicts an increase in exhumation towards the interior of the wedge, with the rate of increase dependent on the degree of internal deformation. Application of the solution to a cross section in the Himalayas shows that in spite of its simplicity the solution provides a good fit to thermochronology data, with a coefficient of dete... more
DOI
https://doi.org/10.31223/X5X316
Subjects
Geology, Tectonics and Structure
Keywords
thermochronology, Himalaya, mountain belts, exhumation
Dates
Published: 2021-03-05 14:59
Last Updated: 2021-03-05 22:59
License
CC BY Attribution 4.0 International
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Conflict of interest statement:
None
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