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References

Amidon, W.H., D.W. Burbank, and G.E. Gehrels (2005), Construction of detrital mineral populations, insights from mixing of U-Pb zircon ages in Himalayan rivers, Basin Research, 17, 463-485.

Beaty, C.B. (1963), Origin of alluvial fans, White Mountains, California and Nevada, Annals of the Association of American Geographers, 53, 516-535.

Brandon, M. T. (1996), Probability density plot for fission-track grain-age samples, Rad. Meas., 26, 5, 663-676.

Brewer, I.D., Burbank, D.W., and Hodges, K.V. (2003), Modelling detrital cooling-age populations: insights from two Himalayan catchments, Basin Research, 15, 305-320.

Conover, W. J. (1999), Practical nonparametric statistics, 584 pp., John Wiley, New York.

Crowder, D. F., Robinson, P. F., and Harris, D. L. (1972), Geologic map of the Benton Quadrangle, Mono County, California and Esmeralda and mineral counties, Nevada, USGS, scale 1:62,500.

Dühnforth, M., Densmore, A.L., Ivy-Ochs, S., Allen, P.A., Kubik, P.W. (2007), Timing and patterns of debris-flow fan deposition on Shepherd and Symmes Creek fans, Owens Valley, California, deduced from cosmogenic $^{10}$Be. Jour. Geophys. Res. Earth Surface (in press).

Galbraith, R. F., and Green, P. F. (1990), Estimating the component ages in a finite mixture, Nucl. Tracks Rad. Meas., 17, 3, 197-206.

Hodges, K.V., K.W. Ruhl, C.W. Wobus, and M.S. Pringle (2005), $^{40}$Ar/$^{39}$Ar Thermochronology of Detrital Minerals, in Low temperature thermochronology: techniques, interpretations, and applications, edited by P.W. Reiners, and T.A. Ehlers, Rev. Mineral. Geochem., 58, 239-257.

Hurford, A.J., and Green, P.F. (1983), The zeta age calibration of fission track dating, Isotope Geosc., 1, 285-317.

Kolmogorov, A. (1933), Sulla determinazione empirica di una legge di distributione, Giornale dell' instituto Italiano degle attuari, 4, 1-11.

McKee, E. H., and Conrad, J. E. (1996), A tale of 10 plutons, revisited; age of granitic rocks in the White Mountains, California and Nevada, Geol. Soc. Am. Bull., 108, 12, 1515-1527.

Ohira, H., Heiguchi, K., Yoshimura, T., Komatsubara, T., Furuno, K., Kudo, H., and Hashimoto, T. (1994), Comparison of two methods of enhancing detection of confined fission tracks in minerals - Ni ion irradiation using a tandem accelerator and fission fragment irradiation using $^{252}$Cf source, J. Geol. Soc. Japan, 100, 2, 129-135.

Reheis, M.C., and T.H. Dixon (1996), Kinematics of the eastern California shear zone: Evidence for slip transfer from Owens and Saline Valley fault zones to Fish Lake Valley fault zone, Geology, 24, 339-342.

Reheis, M.C., and T.L. Sawyer (1997), Late Cenozoic history and slip rates of the Fish Lake Valley, Emigrant Peak, and Deep Springs fault zones, Nevada and California, Geol. Soc. Am. Bull., 109, 280-299.

Rice, J.A. (1995), Mathematical statistics and data analysis, 602 pp., Duxbury Press, Belmont, CA.

Ruhl, K.W., and Hodges, K.V. (2005), The use of detrital mineral cooling ages to evaluate steady state assumptions in active orogens: An example from the central Nepalese Himalaya, Tectonics, 24, doi:10.1029/2004TC001712

Saucedo, G. J., Bedford, D. R., Raines, G. L., Miller, R. J., and Wentworth, C. M. (2000), GIS data for the geologic map of California, compilated by Jennings, C.W. (1977), Cal. Div. Mines Geol..

Silverman, B. W. (1986), Density estimation for statistics and data analysis, 175 pp., Monographs on statistics and applied probability, Chapman and Hall, London, New York.

Smirnov, H. (1939), Sur les écarts de la courbe de distribution empirique, Receuil mathématique (Metematiceskii sbornik), 6, 3-26.

Smirnov, H. (1948), Table for estimating the goodness of fit for empirical distributions, Ann. Math. Stat., 19, 279-281.

Stewart, J. H., (1988), Tectonics of the Walker Lane Belt, western Great Basin: Mesozoic and Cenozoic deformation in a zone of shear, in Rubey Volume, vol. 7, edited by Ernst, W. G., Englewood Cliffs, Prentice-Hall, 683-713.

Stock, J.D., and Montgomery, D.R. (1996), Estimating palaeorelief from detrital mineral age ranges, Basin Research, 8, 317-327.

Stock, G.M., T.A. Ehlers, and K.A. Farley (2006), Where does sediment come from? Quantifying catchment erosion with detrital apatite (U-Th)/He thermochronometry, Geology, 34, 725-728.

Stockli, D. F., Farley, K. A., and Dumitru, T. A. (2000), Calibration of the apatite (U-Th)/He thermochronometer on an exhumed fault block, White Mountains, California, Geology, 28, 11, 983-986.

Stockli, D. F., Dumitru, T. A., McWilliams, M. O., and Farley, K. A. (2003), Cenozoic tectonic evolution of the White Mountains, California and Nevada, Geol. Soc. Am. Bull., 115, 7, 788-816.

Vermeesch, P. (2004), How many grains are needed for a provenance study? Earth Planet. Sci. Lett., 224, 3-4, 441-451.

Vermeesch, P., D. Seward, C. Latkoczy, M. Wipf, D. Günther, and H. Baur (2007), $\alpha$-emitting mineral inclusions in apatite, their effect on (U-Th)/He ages, and how to reduce it, Geochim. Cosmochim. Acta, (in press).


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Next: About this document ... Up: Quantitative geomorphology of the Previous: Acknowledgments
Pieter Vermeesch 2007-01-25