TY - JOUR
T1 - Climatic control on rapid exhumation along the Southern Himalayan Front
AU - Thiede, Rasmus C.
AU - Bookhagen, Bodo
AU - Arrowsmith, Ramon
AU - Sobel, Edward R.
AU - Strecker, Manfred R.
N1 - Funding Information:
The authors would like to thank: A.K. Jain and S. Singh for valuable discussions and logistical support; B. Grasemann, C. Janda, C. Hager, E. Draganits, and J.-C. Vannay for introducing us to the spectacular geology of the Himalaya and granting access to unpublished data; the great Indian mountain guides S. Slathia and T. Tsering for support during fieldwork; and E. Stump, G. Hilley and S. Peacock for discussion and comments on an earlier version of this manuscript. We very much appreciate the reviews by M. Brandon and K. Hodges with detailed comments and suggestions that improved the manuscript significantly. We thank the Deutsche Forschungsgemeinschaft (DFG) for financial support (Grant #STR-11/4), and the DAAD for support of R.T. while at Arizona State University (ASU). [KF]
PY - 2004/6/15
Y1 - 2004/6/15
N2 - Along the Southern Himalayan Front (SHF), areas with concentrated precipitation coincide with rapid exhumation, as indicated by young mineral cooling ages. Twenty new, young (<1-5 Ma) apatite fission track (AFT) ages have been obtained from the Himalayan Crystalline Core along the Sutlej Valley, NW India. The AFT ages correlate with elevation, but show no spatial relationship to tectonic structures, such as the Main Central Thrust or the Southern Tibetan Fault System. Monsoonal precipitation in this region exerts a strong influence on erosional surface processes. Fluvial erosional unloading along the SHF is focused on high mountainous areas, where the orographic barrier forces out > 80% of the annual precipitation. AFT cooling ages reveal a coincidence between rapid erosion and exhumation that is focused in a ∼50-70-km-wide sector of the Himalaya, rather than encompassing the entire orogen. Assuming simplified constant exhumation rates, the rocks of two age vs. elevation transects were exhumed at ∼1.4±0.2 and ∼1.1±0.4 mm/a with an average cooling rate of ∼40-50 °C/Ma during Pliocene-Quarternary time. Following other recently published hypotheses regarding the relation between tectonics and climate in the Himalaya, we suggest that this concentrated loss of material was accommodated by motion along a back-stepping thrust to the south and a normal fault zone to the north as part of an extruding wedge. Climatically controlled erosional processes focus on this wedge and suggest that climatically controlled surface processes determine tectonic deformation in the internal part of the Himalaya.
AB - Along the Southern Himalayan Front (SHF), areas with concentrated precipitation coincide with rapid exhumation, as indicated by young mineral cooling ages. Twenty new, young (<1-5 Ma) apatite fission track (AFT) ages have been obtained from the Himalayan Crystalline Core along the Sutlej Valley, NW India. The AFT ages correlate with elevation, but show no spatial relationship to tectonic structures, such as the Main Central Thrust or the Southern Tibetan Fault System. Monsoonal precipitation in this region exerts a strong influence on erosional surface processes. Fluvial erosional unloading along the SHF is focused on high mountainous areas, where the orographic barrier forces out > 80% of the annual precipitation. AFT cooling ages reveal a coincidence between rapid erosion and exhumation that is focused in a ∼50-70-km-wide sector of the Himalaya, rather than encompassing the entire orogen. Assuming simplified constant exhumation rates, the rocks of two age vs. elevation transects were exhumed at ∼1.4±0.2 and ∼1.1±0.4 mm/a with an average cooling rate of ∼40-50 °C/Ma during Pliocene-Quarternary time. Following other recently published hypotheses regarding the relation between tectonics and climate in the Himalaya, we suggest that this concentrated loss of material was accommodated by motion along a back-stepping thrust to the south and a normal fault zone to the north as part of an extruding wedge. Climatically controlled erosional processes focus on this wedge and suggest that climatically controlled surface processes determine tectonic deformation in the internal part of the Himalaya.
KW - Apatite fission track
KW - Erosion
KW - Exhumation
KW - Geochronology
KW - Himalaya
KW - Precipitation
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U2 - 10.1016/j.epsl.2004.03.015
DO - 10.1016/j.epsl.2004.03.015
M3 - Article
AN - SCOPUS:2942610421
SN - 0012-821X
VL - 222
SP - 791
EP - 806
JO - Earth and Planetary Science Letters
JF - Earth and Planetary Science Letters
IS - 3-4
ER -