『Abstract
Unraveling the relative roles of erosion and tectonics in shaping
the modern topography of active orogens requires datasets documenting
spatial and temporal patterns of exhumation , surface uplift and
climatic forcing throughout orogenic growth. Here we report the
results of biotite 40Ar/39Ar incremental
heating and single-grain laser-fusion experiments from a nearly
vertical, 〜1000 m age-elevation transect in the central Nepalese
Himalaya. Age-elevation relationships constructed from these data
suggest very slow cooling in this part of the Himalayan crystalline
core during the Early Miocene, accelerating to only moderate rates
at 〜10 Ma. If we assume purely vertical exhumation and a steady-state
thermal structure, the exhumation rates implied by these data
are <<0.1 mm/yr prior to 10 Ma and 〜0.5 mm/yr from 〜10-7
Ma. The acceleration in cooling rate at 10 Ma requires a change
in kinematics that may be linked to large-scale changes in climate,
or to more local tectonic perturbations. Although we do not presently
have enough data to assess the relative roles of regional vs.
local drivers, these data provide a new constraint on exhumation
through the Miocene that must be honored by any model of Himalayan
evolution.
Keywords: Himalaya; argon thermochronology; tectonics; climate』
1. Introduction
2. Background
3. Methods
4. Results
4.1. Age-elevation relationships
4.2. Single-grain vs. bulk analyses
5. Discussion
5.1. Are the cooling ages meaningful?
5.2. Change in kinematics at 10 Ma
5.3. Slow cooling before 10 Ma
5.4. A way forward?
6. Conclusions
Acknowledgements
Appendix A. Supplementary data
References