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Rapid denudation of Higher Himalaya during late Pliestocence, evidence from OSL thermochronology

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Geochronometria
Special Issue Title: Proceedings of the 3rd Asia Pacific Conference on Luminescence and Electron Spin Resonance Dating Okayama, Japan, 2012

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[1] Brandon M, Roden-Tice M and Garver J, 1998. Late Cenozoic exhumation of the Cascadia accretionary wedge in the Olympic Mountains, northwest Washington state. Geological Society of America Bulletin 110(8): 985–1009, DOI 10.1130/0016-7606(1998)110〈0985:LCEOTC〉2.3.CO;2. http://dx.doi.org/10.1130/0016-7606(1998)110<0985:LCEOTC>2.3.CO;210.1130/0016-7606(1998)110<0985:LCEOTC>2.3.CO;2Search in Google Scholar

[2] Burbank DW, 2002. Rates of erosion and their implications for exhumation. Mineralogical Magazine 66(1): 25–52, DOI 10.1180/0026461026610014. http://dx.doi.org/10.1180/002646102661001410.1180/0026461026610014Search in Google Scholar

[3] De Sarkar S, Chauhan N, Mathew G, Pande K, and Singhvi AK, 2012. Late Pleistocene rapid denudation, million to thousand year scale. 3rd Asia Pacific Conference on Luminescence and Electron Spin Resonance Dating, Japan. Advances in ESR Applications 29: 22. Search in Google Scholar

[4] Dodson MH, 1973. Closure temperature in cooling geochronological and petrological systems. Contribution to Mineralogy and Petrology 40(3): 259–274, DOI 10.1007/BF00373790. http://dx.doi.org/10.1007/BF0037379010.1007/BF00373790Search in Google Scholar

[5] Ehlers TA, 2005. Crustal thermal processes and the interpretation of thermochronometer data, in Low-Temperature Thermochronology: Techniques, Interpretations, and Applications. In: Reiners PW and Ehlers TA, eds., Low-Temperature Thermochronology: Techniques, Interpretations, Applications. Reviews in Mineralogy and Geochemistry 58: 315–350, DOI 10.2138/rmg.2005.58.12. 10.1515/9781501509575-014Search in Google Scholar

[6] Ehlers TA, Chaudhri T, Kumar S, Fuller CW, Willett SD, Ketcham RA, Bradon MT, Belton DX, Kohn BP, Gleadow AJW, Dunai TJ and Fu FQ, 2005. Computational tools for low-temperature thermochronometer interpretations. Reviews in Mineralogy and Geochemistry 58: 589–622, DOI 10.2138/rmg.2005.58.22. http://dx.doi.org/10.2138/rmg.2005.58.2210.2138/rmg.2005.58.22Search in Google Scholar

[7] Gansser A, 1974. Himalaya. In: Spenser AM, ed., Mesozoic Cenozoic Orogenic Belts: Data for Orogenic Studies. Geological Society of London Special Publication 4: 267–278. 10.1144/GSL.SP.2005.004.01.15Search in Google Scholar

[8] Gansser A, 1983. Geology of the Bhutan Himalaya: Boston, Birkhauser Verlag, 181 p. Search in Google Scholar

[9] Herman F and Braun J, 2006. Fluvial response to horizontal shortening and glaciations: a study in the Southern Alps of New Zealand. Journal of Geophysical Research 111, F01008, DOI 10.1029/2004JF000248. http://dx.doi.org/10.1029/2004JF00024810.1029/2004JF000248Search in Google Scholar

[10] Herman F, Rhodes EJ, Braun J and Heiniger L, 2010. Uniform erosion rates and relief amplitude during glacial cycles in the Southern Alps of New Zealand, as revealed from OSL-thermochronology. Earth Planetary Science Letters 297(1–2): 183–189, DOI 10.1016/j.epsl.2010.06.019. http://dx.doi.org/10.1016/j.epsl.2010.06.01910.1016/j.epsl.2010.06.019Search in Google Scholar

[11] Hodges KV, 2000. Tectonics of the Himalaya and Southern Tibet from two perspectives. Geological Society of America Bulletin 112(3): 324–350, DOI 10.1130/0016-7606(2000)112〈324:TOTHAS〉2.0.CO;2. http://dx.doi.org/10.1130/0016-7606(2000)112<324:TOTHAS>2.0.CO;210.1130/0016-7606(2000)112<324:TOTHAS>2.0.CO;2Search in Google Scholar

[12] Jain M and Ankjaergaard C, 2011. Towards a non-fading signal in feldspar: insight into charge transport and tunnelling from time-resolved optically stimulated luminescence. Radiation Measurements 46(3): 292–309, DOI 10.1016/j.radmeas.2010.12.004. http://dx.doi.org/10.1016/j.radmeas.2010.12.00410.1016/j.radmeas.2010.12.004Search in Google Scholar

[13] Jain M and Singhvi AK, 2001. Limits to depletion of green light stimulated luminescence in feldspars: implication for Quartz dating, Radiation Measurements 33(6): 883–892, DOI 10.1016/S1350-4487(01)00104-4. http://dx.doi.org/10.1016/S1350-4487(01)00104-410.1016/S1350-4487(01)00104-4Search in Google Scholar

[14] Jain M, Choi JH and Thomas PJ, 2008. The ultrafast OSL component in quartz: Origin and implications. Radiation Measurments 43(2–6): 709–714, DOI 10.1016/j.radmeas.2008.01.005. http://dx.doi.org/10.1016/j.radmeas.2008.01.00510.1016/j.radmeas.2008.01.005Search in Google Scholar

[15] Li B and Li SH, 2012. Determining the cooling age using luminescence thermochronology. Tectonophysics 580: 242–248, DOI 10.1016/j.tecto.2012.09.023. http://dx.doi.org/10.1016/j.tecto.2012.09.02310.1016/j.tecto.2012.09.023Search in Google Scholar

[16] Mancktelow NS and Grasemann B, 1997. Time-dependent effects of heat advection and topography on cooling histories during erosion. Tectonophysics 270(3–4): 167–195, DOI 10.1016/S0040-1951(96)00279-X. http://dx.doi.org/10.1016/S0040-1951(96)00279-X10.1016/S0040-1951(96)00279-XSearch in Google Scholar

[17] Madhav MK, 2008. Component Specific Luminescence of Natural Mineral and their application to the dosimetry of Natural Radiation Environment. Unpubl. Ph.D thesis, ML Sukhadia University, Udaipur, India, 129p. Search in Google Scholar

[18] Mathew G, De Sarkar S, Pande K, Jonckheere R, Ratshbacher L and Phukon P, 2013. Late Miocene — Pleistocene enhanced exhumation in the Eastern Himalaya, India (In preparation) Search in Google Scholar

[19] Murray AS and Wintle AG, 2000. Luminescence dating of quartz using an improved single-aliquot regenerative-dose protocol. Radiation Measurements 32(1): 57–73, DOI 10.1016/S1350-4487(99)00253-X. http://dx.doi.org/10.1016/S1350-4487(99)00253-X10.1016/S1350-4487(99)00253-XSearch in Google Scholar

[20] Murray AS and Wintle AG, 2003. The single aliquot regenerative dose protocol: potential for improvements in reliability. Radiation Measurements 37(4–5): 377–381, DOI 10.1016/S1350-4487(03)00053-2. http://dx.doi.org/10.1016/S1350-4487(03)00053-210.1016/S1350-4487(03)00053-2Search in Google Scholar

[21] Plachy AL, 1980. An imporved determination of the internal beta ray dose rate in granite rocks and its effect on thermoluminescence dates. Unpubl. PhD thesis, Washinton University, St. Louis, USA.331p. Search in Google Scholar

[22] Ray L, Bhattacharya A and Roy S, 2007. Thermal conductivity of higher Himalayan crystallines from Garhwal Himalaya, India. Tectonophysics 434(1–4): 71–79, DOI 10.1016/j.tecto.2007.02.003. http://dx.doi.org/10.1016/j.tecto.2007.02.00310.1016/j.tecto.2007.02.003Search in Google Scholar

[23] Reiners PW and Brandon Mark T, 2006. Using thermochronology to understand orogenic erosion. Annual Review of Earth and Planetary Sciences 34: 419–466, DOI 10.1146/annurev.earth.34.031405.125202. http://dx.doi.org/10.1146/annurev.earth.34.031405.12520210.1146/annurev.earth.34.031405.125202Search in Google Scholar

[24] Reiners PW, Ehlers TA and Zeitler PK, 2005. Past, present, and future of thermochronology. In: Reiners PW and Ehlers TA, eds., Low-Temperature Thermochronology: Techniques, Interpretations and Applications. Reviews in Mineralogy and Geochemistry 58: 1–18, DOI 10.2138/rmg.2005.58.1. 10.2138/rmg.2005.58.1Search in Google Scholar

[25] Rhodes EJ, 1990. Optical dating of quartz from sediments. Ph.D. thesis. Oxford. Search in Google Scholar

[26] Roberts HM, 2007. Assessing the effectiveness of the double-SAR protocol in isolating a luminescence signal dominated by quartz. Radiation Measurements 42(10): 1627–1636, DOI 10.1016/j.radmeas.2007.09.010. http://dx.doi.org/10.1016/j.radmeas.2007.09.01010.1016/j.radmeas.2007.09.010Search in Google Scholar

[27] Shuster DL, Ehlers TA, Rusmore ME and Farley KA, 2005. Rapid glacial erosion at 1.8 Ma revealed by 4He/3He thermochronometry. Science 310: 1668–1670, DOI 10.1126/science.1118519. http://dx.doi.org/10.1126/science.111851910.1126/science.1118519Search in Google Scholar

[28] Singarayer J and Bailey RM, 2003. Further investigations of the quartz optically stimulated luminescence components using linear modulation. Radiation Measurements 37(4–5): 451–458, DOI 10.1016/S1350-4487(03)00062-3. http://dx.doi.org/10.1016/S1350-4487(03)00062-310.1016/S1350-4487(03)00062-3Search in Google Scholar

[29] Singhvi AK, Bluszcz A, Bateman M and Someshwararao M, 2001. Luminescence dating of Loess-Paleosol sequences-Methodological Aspects and Paleoclimatic implications Earth-Science Reviews. 54(1–3): 193–221, DOI 10.1016/S0012-8252(01)00048-4. http://dx.doi.org/10.1016/S0012-8252(01)00048-410.1016/S0012-8252(01)00048-4Search in Google Scholar

[30] Stüwe K, White L and Brown R, 1994. The influence of eroding topography on steady-state isotherms: Application to fission track analysis. Earth and Planetary Science Letters 124(1–4): 63–74, DOI 10.1016/0012-821X(94)00068-9. http://dx.doi.org/10.1016/0012-821X(94)00068-910.1016/0012-821X(94)00068-9Search in Google Scholar

[31] Valla PG, Shuster DL and van der Beek PA, 2011. Significant increase in relief of the European Alps during mid-Pleistocene glaciations. Nature Geoscience 4(10): 688–692, DOI 10.1038/ngeo1242. http://dx.doi.org/10.1038/ngeo124210.1038/ngeo1242Search in Google Scholar

[32] Whipp Jr. DM, Ehlers TA, Blythe AE, Huntington KW, Hodges KV and Burbank DW, 2007. Plio-Quaternary exhumation history of the central Nepalese Himalaya: 2. Thermokinematic and thermochronometer age prediction model. Tectonics 26(3): TC3003, DOI 10.1029/2006TC001991. http://dx.doi.org/10.1029/2006TC00199110.1029/2006TC001991Search in Google Scholar

[33] Whipple KX, 2009. The influence of climate on the tectonic evolution of mountain belts. Nature Geoscience 2(2): 97–105, DOI 10.1038/ngeo413. http://dx.doi.org/10.1038/ngeo41310.1038/ngeo413Search in Google Scholar

[34] Willett SD and Brandon MT, 2002. On steady states in mountain belts. Geology 30(2): 175–178, DOI 10.1130/0091-7613(2002)030〈0175:OSSIMB〉2.0.CO;2. http://dx.doi.org/10.1130/0091-7613(2002)030<0175:OSSIMB>2.0.CO;210.1130/0091-7613(2002)030<0175:OSSIMB>2.0.CO;2Search in Google Scholar

[35] Yin A, Dubey CS, Kelty TK, Gehrels GE, Chou CY, Grove M and Lovera O, 2006. Structural evolution of the Arunachal Himalaya and implications for asymmetric development of the Himalayan orogen. Current Science 90(2): 195–206. Search in Google Scholar

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