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Rates of erosion and their implications for exhumation

Published online by Cambridge University Press:  05 July 2018

D. W. Burbank
D. W. Burbank*
Affiliation:
Institute for Crustal Studies, University of California, Santa Barbara, CA 93106, USA
*
*E-mail: burbank@crustal.ucsb.edu
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Abstract

At time-scales of 102 to 105 years, erosion by rivers, landslides and glaciers can exceed 5 mm/y. Sustained denudation at these rates is sufficient to account for many of the rapid rates of unloading or cooling that are revealed by geobarometric or thermochronologic studies. Because feedbacks exist among many surface processes, determinations of erosion rates on a few geomorphic processes can be adequate to estimate mean rates across an entire landscape. Rates of fluvial and glacial incision exert a dominant control on landscape lowering, because these rates set the local base level and modulate the flux from adjacent hillslopes. When rates of deformation are sufficiently rapid and sustained, a collisional orogen approaches a dynamic equilibrium or topographic steady state. Due to variations in erosion rates as a function of Late Cenozoic climate changes, such a steady state should be defined at time-scales longer than one climate cycle. During dynamic equilibrium, the geomorphic system displays a predictable configuration of interacting rivers, hillslopes and glaciated process zones. A dynamic equilibrium appears to prevail near Nanga Parbat, Pakistan, and the Southern Alps of New Zealand, where spatial variations in geomorphic erosion rates mimic variations in bedrock cooling rates at time-scales of 106 y.

Keywords

erosionexhumationdenudationNanga ParbatSouthern AlpsNew Zealand
Type
Research Article
Information
Mineralogical Magazine , Volume 66 , Issue 1 , February 2002 , pp. 25 - 52
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 2002

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References

Allen, P.A. (1997) Earth Surface Processes. Blackwell Science, Oxford, UK.CrossRefGoogle Scholar
Amato, J.M., Johnson, C.M., Baumgartner, L.P. and Beard, B.L. (1999) Rapid exhumation of the Zermatt-Saas ophiolite deduced from high-precision Sm–Nd and Rb–Sr geochronology. Earth and Planetary Science Letters, 171, 425–438.CrossRefGoogle Scholar
Anderson, R.S. (1994) Evolution of the Santa Cruz Mountains, California, through tectonic growth and geomorphic decay. Journal of Geophysical Research, 99, 20, 161-20,179.CrossRefGoogle Scholar
Anderson, R.S. and MacGregor, K.C. (1998) The role of glacial erosion in mountain range evolution. EOS (Transactions of the American Geophysical Union), 79, 337.Google Scholar
Andrews, D.J. and Hanks, T.C. (1985) Scarps degraded by linear diffusion: inverse solution for age. Journal of Geophysical Research, 90, 10193–10208.CrossRefGoogle Scholar
Balanyá, J.C., García-Dueñas, V., Azañon, J.M. and Sánchez-Gómez, M. (1997) Alternating contractional and extensional events in the Alpujarride nappes of the Alborán Domain (Betics, Gibraltar Arc). Tectonics, 16, 226–238.CrossRefGoogle Scholar
Beaumont, C., Fullsack, P. and Hamilton, J. (1992) Erosional control of active compressional orogens. Pp. 1–18 in: Thrust Tectonics. (McClay, K.R., editor). Chapman & Hall, London.Google Scholar
Bierman, P. (1994) Using in situ produced cosmogenic isotopes to estimate rates of landscape evolution: a review from the geomorphic perspective. Journal of Geophysical Research, 99, 13, 885-13,896.CrossRefGoogle Scholar
Brandon, M.T., Roden-Tice, M.K. and Garver, J.I. (1998) Late Cenozoic exhumation of the Cascadia accretionary wedge in the Olypmic Mountains, northwest Washington State. Geological Society of America Bulletin, 110, 985–1009.2.3.CO;2>CrossRefGoogle Scholar
Brocklehurst, S.H. and Whipple, K.X. (2002) Glacial erosion and relief production in the eastern Sierra Nevada, California. Geomorphology. (in press).CrossRefGoogle Scholar
Brozovic, N., Burbank, D.W. and Meigs, A.J. (1997) Climatic limits on landscape development in the northwestern Himalaya. Science, 276, 571–574.CrossRefGoogle Scholar
Bull, W.B. (1991) Geomorphic Responses to Climatic Change. Oxford University Press, London.Google Scholar
Bull, W.B. and Cooper, A.F. (1986) Uplifted marine terraces along the Alpine fault, New Zealand. Science, 234, 1225–1228.CrossRefGoogle ScholarPubMed
Burbank, D.W., Leland, J., Fielding, E., Anderson, R.S., Brozovic, N., Reid, M.R. and Duncan, C. (1996) Bedrock incision, rock uplift and threshold hillslopes in the northwestern Himalaya. Nature, 379, 505–510.CrossRefGoogle Scholar
Burbank, D.W., Lavé, J., Meigs, A.J., Fielding, E.F. and Blythe, A.E. (1998) Consistent long and short-term denudatio n patterns in the San Gabriel and Himalayan Mountains. EOS (Transactions of the American Geophysical Union), 79, 338.Google Scholar
Burchfiel, B.D., Zhileng, C., Hodges, K.V., Yuping, L., Royden, L.H., Changrong, D. and Jiene, X. (1992) The South Tibetan Detachment System, Himalayan Orogen: Extension Contemporaneous with and Parallel to Shortening in a Collisional MountainBelt. Geological Society of America, Special Paper 269.Google Scholar
Butler, R.W.H., Harris, N.B.W. and Whittington, A.G. (1997) Interactions between deformation, magmatism and hydrothermal activity during active crustal thickening: a field example from Nanga Parbat, Pakistan Himalayas. Mineralogical Magazine, 61, 37–52.CrossRefGoogle Scholar
Chamberlain, C.P. and Poage, M.A. (2000) Reconstructing the paleotopography of mountain belts from the isotopic composition of authigenic minerals. Geology, 28, 115–118.2.0.CO;2>CrossRefGoogle Scholar
Chamberlain, C.P., Poage, M.A., Craw, D. and Reynolds, R.C. (1999) Topographic development of the Southern Alps recorded by the isotopic composition of authigenic clay minerals, South Island, New Zealand. Chemical Geology, 155, 279–294.CrossRefGoogle Scholar
Church, M. and Slaymaker, O. (1989) Disequilibrium of Holocene sediment yield in glaciated British Columbia. Nature, 337, 452–454.CrossRefGoogle Scholar
Clark, D.H., Clark, M.M. and Gillespie, A.R. (1994) Debris-covered glaciers in the Sierra Nevada, California and their implications for snowline reconstructions. Quaternary Research, 41, 139–153.CrossRefGoogle Scholar
Craw, D., Koons, P.O., Winslow, D., Chamberlain, C.P. and Zeitler, P. (1994) Boiling fluids in a region of rapid uplift, Nanga Parbat massif, Pakistan. Earth and Planetary Science Letters, 128, 169–182.CrossRefGoogle Scholar
Edwards, M.A., Kidd, W.S.F., Khan, M.A. and Schneider, D.A. (2000) Tectonics of the SW margin of the Nanga Parbat-Haramosh Massif. Pp. 77–100 in: Tectonics of the Nanga Parbat Syntaxis and the Western Himalay. (Khan, M.A., Treloar, P.J., Searle, M.P. and Jan, M.Q., editors). Special Publication, 170. Geological Society, London.Google Scholar
Fitzgerald, P.G., Sorkhabi, R.B., Redfield, T.F. and Stump, E. (1995) Uplift and denudation of the central Alaska Range: a case study in the use of apatite fission track thermochronology to determine absolute uplift parameters. Journal of Geophysical Research, 100, 20, 175-20,191.CrossRefGoogle Scholar
Flinch, J.F. (1996) Accretion and extensional collapse of the external Western Rif (Northern Morocco). Pp. 61–85. in: Peri-Tethys Memoir 2: Structure and Prospects of Alpine Basins and Forelands. (Ziegler, P.A. and Horváth, F., editors). Mémoires du Muséum National d'Histoire Naturelle, 170, Paris.Google Scholar
Forest, C.E., Wolfe, J.A., Molnar, P. and Emanuel, K.A. (1999) Paleoaltimetry incorporating atmospheric physics and botanical estimates of paleoclimate. Geological Society of America Bulletin, 111, 1497–511.2.3.CO;2>CrossRefGoogle Scholar
Fort, M. (1987) Sporadic morphogenesis in a continental subduction setting: an example from the Annapurna Range, Nepal Himalaya. Zeitschrift für Geomorphologie, 63, 9–36.Google Scholar
Foster, D.A., Gleadow, A.J.W. and Mortiner, G. (1994) Rapid Pliocene exhumation in the Karakoram (Pakistan), revaled by fission-track thermochronology of the K2 gneiss. Geology, 22, 19–22.2.3.CO;2>CrossRefGoogle Scholar
Foster, D.A. and John, B.E. (1999) Quantifying tectonic exhumation in an extensional orogen with thermochronology: examples from the southern Basin and Range Province. Pp. 343–364 in: Exhumation Processes: Normal Faulting, Ductile Flow and Erosion. (Ring, U., Brandon, M.Y., Lister, G.S. and Willett, S.D., editors). Special Publication 154. Geological Society, London.Google Scholar
Galy, A. and France-Lanord, C. (2001) Higher erosion rates in the Himalaya: Geochemical constraints on riverine fluxes. Geology, 29, 23–26.2.0.CO;2>CrossRefGoogle Scholar
Gardner, J.S. and Jones, N.K. (1993) Sediment transport and yield at the Raikot Glacier, Nanga Parbat, Punjab Pakistan. Pp. 184–197 in: Himalaya to the Sea: Geology, Geomorphology and the Quaternar. (Shroder, J.F. Jr., editor). Routledge, London.CrossRefGoogle Scholar
Gregory, K. (1994) Palaeoclimate and palaeoelevation of the 35 Ma Florrisant flora, Front Range, Colorado. Palaeoclimatology, 1, 23–57.Google Scholar
Guillot, S., Cosca, M., Allemand, P. and Le Fort, P. (1999) Contrasting metamorphic and geochronologic evolution along the Himalayan belt. Geological Society of America Special Paper, 328, 117–128.Google Scholar
Hack, J.T. (1960) Interpretation of erosional topography in humid temperate regions. American Journal of Science, 258-A, 80–97.Google Scholar
Hack, J.T. (1975) Dynamic equilibrium and landscape evolution. Pp. 87–102 in: Theories of Landform Evolution. (Melhorn, W.N. and Flemal, R.C., editors). Allen and Unwin, Boston, USA.Google Scholar
Hacker, B.R., Calvert, A., Zhang, R.Y., Ernst, G.W. and Liou, J.G. (in review) Ultra-Rapid Exhumation of Ultrahigh-Pressure Diamond-Bearing Metasedimentary Rocks of the Kokchetav Massif. Earth and Planetary Science Letters. Google Scholar
Hallet, B. (1979) A theoretical model of glacial abrasion. Journal of Glaciology, 23, 39–50.Google Scholar
Hallet, B., Hunter, L. and Bogen, J. (1996) Rates of erosion and sediment evacuation by glaciers: a review of field data and their implications. Global Planetary Change, 12, 213–235.CrossRefGoogle Scholar
Hanks, T.C., Bucknam, R.C., LaJoie, K.R. and Wallace, R.E. (1984) Modification of wave-cut and faulting controlled landforms. Journal of Geophysical Research, 89, 5771–5790.CrossRefGoogle Scholar
Harbor, J.M., Hallet, B. and Raymond, C.F. (1988) A numerical model of landform development by glacial erosion. Nature, 333, 347–349.CrossRefGoogle Scholar
Harrison, T.M., Ryerson, F.J., Le Fort, P., Yin, A., Lovera, O.M. and Catlos, E.J. (1997) A late Miocene-Pliocene origin for the central Himalayan inverted metamorphism. Earth and Planetary Science Letters, 146, El–E7.Google Scholar
Heimsath, A.M. (1999) The Soil Production Function. PhD thesis, University of California, Berkeley.Google Scholar
Heimsath, A.M., Dietrich, W.E., Nishiizumi, K. and Finkel, R.C. (1997) The soil production function and landscape equilibrium. Nature, 388, 358–361.CrossRefGoogle Scholar
Heimsath, A.M., Dietrich, W.E., Nishiizumi, K. and Finkel, R.C. (1999) Cosmogenic nuclides, topography and the spatial variation of soil depth. Geomorphology, 27, 151–172.CrossRefGoogle Scholar
Horton, R.E. (1945) Erosional development of streams and their drainage basins, hydrophysical approach to quantitative morphology. Geological Society of America Bulletin, 56, 275–370.CrossRefGoogle Scholar
House, M.A., Wernicke, B.P. and Farley, K.A. (1998) Dating topography of the Sierra Nevada, California, using apatite (U-Th)/He ages. Nature (London), 396(6706), 66–69.CrossRefGoogle Scholar
Hovius, N., Stark, C.P. and Allen, P.A. (1997) Sediment flux from a mountain belt derived by landslide mapping. Geology, 25, 231–234.2.3.CO;2>CrossRefGoogle Scholar
Hovius, N., Stark, C.P., Chu, H.T. and , J.-C.L. (2000) Supply and removal of sediment in a landslide-dominated mountain belt: Central Range, Taiwan. Journal of Geology, 108, 73–90.CrossRefGoogle Scholar
Howard, A.D., Dietrich, W.E. and Seidl, M.A. (1994) Modeling fluvial erosion on regional to continental scales. Journal of Geophysical Research, 99, 13, 971-13,986.CrossRefGoogle Scholar
Hubbard, M.S., Spencer, D.A. and West, D.P. (1995) Tectonic exhumation of the Nanga Parbat massif, northern Pakistan. Earth and Planetary Science Letters, 133, 213–225.CrossRefGoogle Scholar
Humphrey, N.F. and Raymond, C.F. (1994) Hydrology, erosion and sediment production in a surging glacier: The Variegated Glacier surge, 1982–1983. Journal of Glaciology, 40, 539–552.CrossRefGoogle Scholar
Isacks, B., Masek, J., Fielding, E., Jordan, T., Bloom, A., Cook, K. and Anonymous (1994) Tectonic/climatic erosion machines. Geological Society of America Abstracts with Program, 26, 382–383.Google Scholar
Kamp, P.J.J. and Tippett, J.M. (1993) Dynamics of Pacific plate crust in the South Island (New Zealand) zone of oblique continent-continent convergence. Journal of Geophysical Research, 98, 16, 107-16, 118.CrossRefGoogle Scholar
Kooi, H. and Beaumont, C. (1996) Large-scale geomorphology: classical concepts reconciled and integrated with contemporary ideas via a surface processes model. Journal of Geophysical Research, 101, 3361–3386.CrossRefGoogle Scholar
Koons, P.O. (1989) The topographic evolution of collisional mountain belts: A numerical look at the Southern Alps, New Zealand. American Journal of Science, 1041–1069.CrossRefGoogle Scholar
Koons, P.O. (1998) Big mountains, big rivers, and hot rocks. EOS (Transactions of the American Geophysical Union), 79, 908.Google Scholar
Kutzbach, J.E., Prell, W.L. and Ruddiman, W.F. (1993) Sensitivity of Eurasian climate to surface uplift of the Tibetan Plateau. Journal of Geology, 100, 177–190.CrossRefGoogle Scholar
Lavé, J. and Avouac, J. P. (2000) Active folding of fluvial terraces across the Siwalik Hills, Himalaya of central Nepal. Journal of Geophysical Research, 105, 5735–5770.CrossRefGoogle Scholar
Leland, J., Reid, M.R., Burbank, D.W., Finkel, R. and Caffee, M. (1998) Late Pleistocene history of bedrock incision and differential uplift along the Indus River near Nanga Parbat, Pakistan Himalaya, from 10Be and 26A1 exposure age dating of bedrock straths. Earth and Planetary Science Letters, 54, 93–105.CrossRefGoogle Scholar
MacGregor, K.C., Anderson, R.S., Anderson, S.P. and Waddington, E.D. (1998) Glacially driven evolution of long valley profiles and implications for alpine landscape evolution. EOS (Transactions of the American Geophysical Union), 79, 337.Google Scholar
Martinson, D.G., Pisias, N.G., Hays, J.D., Imbrie, J., Moore, T.C. and Shackleton, N.J. (1987) Age dating and orbital theory of the ice ages: Development of a high resolution 0 to 300,000–year chronostratigraphy. Quaternary Research, 27, 1–29.CrossRefGoogle Scholar
Meigs, A. (1998) Bedrock landsliding forced by deglaciation: Three possible examples from the Chugach/St. Elias Range, Alaska. EOS (Transactions of the American Geophysical Union), 79, 337.Google Scholar
Meltzer, A., Sarker, G., Seeber, L. and Armbruster, J. (1998) Snap, crackle, pop! Seismicity and crustal structure at Nanga Parbat, Pakistan, Himalaya. EOS (Transactions of the American Geophysical Union), 79, 909.Google Scholar
Milliman, J.D. (1997) Fluvial sediment discharge to the sea and the importance of regional tectonics. Pp. 240–258 in: Tectonic Uplift and Change. (Ruddiman, W.F., editor). Plenum, New York.Google Scholar
Milliman, J.D. and Syvitski, J.P.M. (1992) Geomorphic/tectonic control of sediment discharge to the ocean: The importance of small mountainous rivers. Journal of Geology, 100, 525–544.CrossRefGoogle Scholar
Montgomery, D.R. and Dietrich, W.E. (1994) A physically based model for the topographic control on shallow landsliding. Water Resources Research, 30, 1153–1171.CrossRefGoogle Scholar
Nishiizumi, K., Kohl, C.P., Arnold, J.R., Dorn, R., Klein, J., Fink, D., Middleton, R. and Lal, D. (1993) Role of in situ. cosmogenic nuclides 10Be and 26Al in the study of diverse geomorphic processes. Earth Surface Processes and Landforms, 18, 407–425.CrossRefGoogle Scholar
Ohmori, H. (1992) Morphological characteristics of the scar created by large-scale rapid mass movement. Japanese Geomorphology Union Transactions, 13, 185–202.Google Scholar
Platt, J.P. (1986) Dynamics of orogenic wedges and the uplift of high-pressure metamorphic rocks. Geological Society of America Bulletin, 97, 1037–1053.2.0.CO;2>CrossRefGoogle Scholar
Porter, S.C. (1989) Some geological implication of average Quaternary glacial conditions. Quaternary Research, 32, 245–261.CrossRefGoogle Scholar
Roering, J.J., Kirchner, J.W. and Dietrich, W.E. (1999) Evidence for nonlinear, diffusive sediment transport on hillslopes and implications for landscape morphology. Water Resources Research, 35, 853–870.CrossRefGoogle Scholar
Rosenbloom, N.A. and Anderson, R.S. (1994) Hillslope and channel evolution in a marine terraced landscape, Santa Cruz, California. Journal of Geophysical Research, 99, 14, 013-14,029.CrossRefGoogle Scholar
Rubatto, D. and Hermann, J. (2001) Exhumation as fast as subduction? Geology, 29, 3–6.2.0.CO;2>CrossRefGoogle Scholar
Sahagian, D.L. and Maus, J.E. (1994) Basalt vesicularity as a measure of atmospheric pressure and palaeo-elevation. Nature, 372, 449–451.CrossRefGoogle Scholar
Schmidt, K.M. and Montgomery, D.R. (1995) Limits to relief. Science, 270, 617–620.CrossRefGoogle Scholar
Schmidt, K.M. and Montgomery, D.R. (1996) Rock mass strength assessment for bedrock landsliding. Environmental Engineering Geoscience, 2, 325–338.CrossRefGoogle Scholar
Schneider, D.A., Edwards, M.A., Kidd, W.S.F., Asif Khan, M., Seeber, L. and Zeitler, P.K. (1999) Tectonics of Nanga Parbat, western Himalaya; synkinematic plutonism within the doubly vergent shear zones of a crustal-scale pop-up structure. Geology, 27, 999–1002.2.3.CO;2>CrossRefGoogle Scholar
Schumm, S.A., Mosley, M.P. and Weaver, W.E. (1987) Experimental Fluvial Geomorphology. 413 pp. John Wiley & Sons, New York.Google Scholar
Searle, M.P. (1996) Cooling history, erosion, exhumation and kinematics of the Himalaya-Karakoram-Tibet orogenic belt. Pp. 110–137 in: Asian Tectonics. (Yin, A. and Harrison, M.A., editors). Cambridge University Press, Cambridge, UK.Google Scholar
Seeber, L. and Pêcher, A. (1998) Strain partitioning along the Himalayan arc and the Nanga Parbat antiform. Geology, 26, 791–794.2.3.CO;2>CrossRefGoogle Scholar
Seidl, M.A., Dietrich, W.E. and Kirchner, J.W. (1994) Longitudinal profile development into bedrock: an analysis of Hawaiian channels. Journal of Geology, 102, 457–474.CrossRefGoogle Scholar
Selby, M.J. (1982) Controls on the stability and inclination of hillslopes on hard rock. Earth Surface Processes and Landforms, 7, 449–467.CrossRefGoogle Scholar
Sklar, L. and Dietrich, W.E. (1998) River longitudinal profiles and bedrock incision models stream power and the influence of sediment supply. Pp. 237–260 in: River Over Rock: Fluvial Processes in Bedrock Channel. (Tinkler, K.J. and Wohl, E.E., editors). American Geophysical Union Geophysical Monograph, 107, Washington, D.C. CrossRefGoogle Scholar
Slingerland, R. and Snow, R.S. (1988) Stability analysis of a rejuvenated fluvial system. Zeitschrift für Geomorphologie, 67, 93–102.Google Scholar
Small, E.E., Anderson, R.S., Repka, J.L. and Finkel, R. (1997) Erosion rates of alpine bedrock summit surfaces deduced from in situ 10Be and 26Al. Earth and Planetary Science Letters, 150, 413–425.CrossRefGoogle Scholar
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, 63–74.CrossRefGoogle Scholar
Thomson, S.N., Stöckhert, B. and Brix, M.R. (1999) Miocene high-pressure metamorphic rocks of Crete, Greece: rapid exhumation by buoyant excape. Pp. 87–107 in: Exhumation Processes: Normal Faulting, Ductile Flow and Erosion. (Ring, U., Brandon, M.Y., Lister, G.S. and Willett, S.D., editors). Special Publication 154. Geological Society, London.Google Scholar
Tinkler, K.J. and Wohl, E.E. (1998) River Over Rock: Fluvial Processes in Bedrock Channels. American Geophysical Union, Geophysical Monograph 107, Washington, D.C. CrossRefGoogle Scholar
Tippett, J.M. and Kamp, P.J.J. (1993) Fission track analysis of the Late Cenozoic vertical kinematics of continental Pacific crust, South Island, New Zealand. Journal of Geophysical Research, 98, 16. 119-16, 148.CrossRefGoogle Scholar
Tippett, J.M. and Kamp, P.J.J. (1995) Quantitative relationships between uplift and relief parameters for the Southern Alps, New Zealand, as determined by fission track analysis. Earth Surface Processes and Landforms, 20, 153–175.CrossRefGoogle Scholar
Weiland, R.J. and Cloos, M. (1996) Pliocene-Pleistocene asymmetric unroofing of the Irian fold belt, Irian Jaya, Indonesia: Apatite fission-track thermochronology. Geological Society of America Bulletin, 108, 1438–1449.2.3.CO;2>CrossRefGoogle Scholar
Wernicke, B. (1992) Cenozoic extensional tectonics of the U.S. Cordillera. Pp. 553–581 in: The Geology of North America G-3. (Burchfiel, B.C., Lipman, P.W. and Zoback, M.L., editors). Geological Society of America, Boulder, CO, USA.Google Scholar
Whipple, K.E., Kirby, E. and Brocklehurst, S.H. (1999) Geomorphic limits to climate-induced increases in topographic relief. Nature, 401, 39–43.CrossRefGoogle Scholar
Willett, S.D. (1999) Orogeny and orography: the effects of erosion on the structure of mountain belts. Journal of Geophysical Research, 104, 28, 957-28,982.CrossRefGoogle Scholar
Winslow, D.W., Zeitler, P.K., Chamberlain, C.P. and Williams, I.S. (1996) Geochronologic constraints on syntaxial development in the Nanga Parbat region, Pakistan. Tectonics, 15, 1292–1308.CrossRefGoogle Scholar
Wolf, R.A., Farley, K.A. and Kass, D.M. (1998) Modeling of the temperature sensitivity of the apatite (U-Th)/He thermochronometer. Chemical Geology, 148, 105–114.CrossRefGoogle Scholar
Wolfe, J.A., Schorn, H.E., Forest, C.E. and Molnar, P. (1997) Paleobotanical evidence for high altitudes in Nevada during the Miocene. Science, 276, 1672–1675.CrossRefGoogle Scholar
Zeitler, P.K. (1985) Himalaya, Pakistan. Tectonics, 4, 127–151.CrossRefGoogle Scholar
Yamanaka, H. and Iwata, S. (1982) River terraces along the middle Kali Gandaki and Marsyandi Khola, central Nepal. Journal of the Nepal Geological Society, 2, 95–112.Google Scholar
Zeitler, P.K. (1985) Cooling history of the NW Himalaya, Pakistan. Tectonics, 4, 127–151.CrossRefGoogle Scholar
Zeitler, P.K., Meltzer, A.S., Koons, P.O., Craw, D., Hallet, B., Chamberlain, C.P., Kidd, W.S.F., Park, S.K., Seeber, L., Bishop, M. and Shroder, J. (2001) Erosion, Himalayan Geodynamics, and the Geomorphology of Metamorphism. Geological Society of America Today, 11, 4–9.Google Scholar