Climatic control on rapid exhumation along the Southern Himalayan Front

@article{citeulike:3065356, abstract = {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.}, author = {Thiede, Rasmus C. and Bookhagen, Bodo and Arrowsmith, Ram\'{o}n J. and Sobel, Edward R. and Strecker, Manfred R.}, citeulike-article-id = {3065356}, doi = {10.1016/j.epsl.2004.03.015}, journal = {Earth and Planetary Science Letters}, keywords = {building, erosion, incision, mountain, precipitation, river, uplift}, month = {June}, number = {3-4}, pages = {791--806}, posted-at = {2008-07-31 12:29:42}, priority = {2}, title = {Climatic control on rapid exhumation along the Southern Himalayan Front}, url = {http://dx.doi.org/10.1016/j.epsl.2004.03.015}, volume = {222}, year = {2004} }

TY - JOUR ID - citeulike:3065356 L3 - citeulike-article-id:3065356 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. IS - 3-4 JF - Earth and Planetary Science Letters EP - 806 TI - Climatic control on rapid exhumation along the Southern Himalayan Front VL - 222 SP - 791 KW - building KW - erosion KW - incision KW - mountain KW - precipitation KW - river KW - uplift AU - Thiede, Rasmus AU - Bookhagen, Bodo AU - Arrowsmith, Ramón AU - Sobel, Edward AU - Strecker, Manfred PY - 2004/06/15/ UR - http://dx.doi.org/10.1016/j.epsl.2004.03.015 ER -