[1]
B.B. Mandelbrot. "The fractal geometry of nature",Freeman, New York, 1982 , pp. 468l.
Google Scholar
[2]
R.E. Horton. "Drainage basin characteristics",Transactions of the American Geophysical Union (AGU) 13, 1932, pp.350-370.
Google Scholar
[3]
R.E. Horton. "Erosional development of streams and their drainage basins: hydrophysical approach to quantitative geomorphology", Geol. Soc. Am. Bull, 1945, pp.275-370.
DOI: 10.1130/0016-7606(1945)56[275:edosat]2.0.co;2
Google Scholar
[4]
P. La Barbera, R. Rosso. "On the fractal dimension of stream networks", Water Resour, Res. 25, 1989, pp.735-741.
DOI: 10.1029/wr025i004p00735
Google Scholar
[5]
M. Fiorentino, G. Oliveto and A. Rossi. "Alcuni aspetti del controllo energetico ed idrologico sulla geometria delle reti e delle sezioni fluviali. Parte prima: controlloidrologico, Atti del XXVIII Convegno di Idraulica e Costruzioni Idrauliche: Potenza", Editoriale Bios Cosenza,1, 2002, pp.71-78.
Google Scholar
[6]
C. Cudennec, Y. Fouad, G.I. Sumarjo and J. Duchesne. "A geomorphological explanation of the unit hydrograph concept",. Hydrol. Process, 2004, pp.603-621.
DOI: 10.1002/hyp.1368
Google Scholar
[7]
A.T. Hjelmfelt."Fractals and the river-length catchment-area ratio",Water Resour. Bull.24, 1988, pp.455-459.
DOI: 10.1111/j.1752-1688.1988.tb03005.x
Google Scholar
[8]
D.G. Tarboton, R.L. Bras and I. Rodriguez-Iturbe. "The fractal nature of river networks", Water Resour,1988, pp.1317-1322.
DOI: 10.1029/wr024i008p01317
Google Scholar
[9]
M. Veltri, P. Veltri, M. Maiolo. "On the fractal description of natural channel networks", J. Hydrol, 1996, pp.137-144.
DOI: 10.1016/s0022-1694(96)03091-0
Google Scholar
[10]
D.G. Tarboton. "Fractal river networks, Horton's laws and Tokunaga cyclicity", J. Hydrol. 1996, pp.105-117.
DOI: 10.1016/s0022-1694(96)03089-2
Google Scholar
[11]
V. Nikora, V.B. Sapozhinov and D.A. Noever. "Fractal geometry of individual river channels and its computer simulation",. Water Resour, 1993, pp.3561-3568.
DOI: 10.1029/93wr00978
Google Scholar
[12]
D.J. Schuller, A.R. Rao and G.D. Jeong. "Fractal characteristics of dense stream networks", J. Hydrol, 2001, pp.1-16.
Google Scholar
[13]
S.G. De Bartolo, M. Veltri, L. Primavera. "Estimated generalized dimensions of river networks", J. Hydrol, 2006, pp.181-191.
DOI: 10.1016/j.jhydrol.2005.02.033
Google Scholar
[14]
X.H. Shen, L.J. Zou, G.F. Zhang, N. Sua, W.Y. Wu and S.F. Yang. "Fractal characteristics of the main channel of Yellow River and its relation to regional tectonic evolution",Geomorphology, 2011, pp.64-70.
DOI: 10.1016/j.geomorph.2010.12.007
Google Scholar
[15]
L.F. Richardson. "The Problem of Contiguity: An Appendix of Statistics of Deadly Quarrels", General Systems: Yearbook of the Society for General Systems Reserch 6, Ann Arbor, 1961,pp.139-187.
Google Scholar
[16]
P. Grassberger. "On efficient box counting algorithms", Int. J. Mod. Phys, 1983, pp.515-523.
Google Scholar
[17]
B.B. Mandelbrot. "How long is the coast of Britain? Statistical self-similarity and fractional dimension", Science ,1967, pp.636-638.
DOI: 10.1126/science.156.3775.636
Google Scholar
[18]
R.S. Snow. "Fractal sinuosity of stream channels", Pure Appl. Geophys, 1989, pp.99-10.
Google Scholar
[19]
A. Beauvais, D.R Montgomery. "Influence of valley type on the scaling properties of river planforms", Water Resour, 1996, pp.1441-1448.
DOI: 10.1029/96wr00279
Google Scholar