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(1) Harms, J.C. et al.,1975, Depositional environments as interpreted from prim-ary sedimentary strutures and stratification sequences:Tulsa, Okla.,Soc.Econ.paleontologists and bfineralolgists, Dallas,Short Course NO.2.LectLre Notes,161.
(2) Harms, J.C.&Fahnestock, R.K.,1965, Stratification, bedforms, and flog- ph- enomena(with an eyample from the Rio Grande),SEPM.Spe;ial Publication 121977, P.84-115.
(3) Harms, J.C.,1979, Primary sedimentary- strutures, Am.Rea Earth Plaret.Sci.M.7,227-298.
(4) Vanoni,V,A.,1974。Factors determining bed forms of allu、·ial streams,Proc.Am.Soc.civil. Eng.,T.Hydraul.Di}".,100, 363-377.
(5) Simons, 1961,Forms of bed rough in alluvial channels,.Amer.Soc.Ciuil.Eng.proc 87(3),87-105.
(6) Simons, D.B.,Richardsons, E.V1962,Resistance to flow in alluvial channelsAm.Soc.Cio.Eregrs.Trana.127, 927-953.
(7) W iddleton, G.V,1977, Introduction-process in hpdraulie interpretation o` sedi- mentar5- structures, SEPhS.Reprint Series Number 3,1-15.
(8) Kennedy, J.F.,1963, The mechanics of dunes and antidunes in erodible-bed chaannels. J.Fluid Mech.,16, 521-544.
(9) lilein,G.D.,1970, Deposional and disperasal dynamics of intcrtidal sand bars.J.Sed.Petro.,40, 1095-11?7.
(10)Athaullan, M.,1968, Prediction of bed forms in erodible channels. phD Disse- rtation, Colorado State Univ.,F ort C ollins C olorado, 161.
(11) Allen,J.R.L.,1970, Aquantitative model of grain size and sedimentary struc-tures is lateral deposits, Geo.J.7,129-146.
(12) Alan.jr.J.,1965,Hydraulic fators controlling the shape of laminae in laboratory deltas, J.Sed.Petro.,35(4),777-791.
(13) Picard, M.D.&High, L.R.,1973, Sedimentary structures of ephemeral strea-ms,Developments in Sedimentology 17, Elsevier Sci.Pub.Co.,Amsterdam,223p.
(14) Pettijohn, Potter, Siever, 1972, Sand and sandstone,New York. Sprinser-Var- lag, 618p。
(15) Visher, G.S.,1969, Grain size distribution and depositional processes,J.Sed. Pet.39, 1074-1106。
(16) Allen, J.R.L1964, Studies in: flurviatile sedirnentation. Sedimer:tology, 3, 163-198。
(17) Simons, channels, D.B.et a1., 1965, Sedimentary structures generated by flow in alluvial SEMP.Special Publication 12, 34-52.
(18) Middleton,G.V.,1977,Sedimentary process:hydraulic interpretation of primary sedimentary structures, SEPM.Reprint Series Number 3,400p.
(19) Nanson, G.C.,1980, Point bar and floodplain formation of the meandering Be-atton River, northeastern British Columbia, Canada, Sedimentology, 27(1),3一31。
(20) Kennedy, J.F.,Stationary waves and anti-dunes in alluvial channels,Rep KH- R一2,Keck Lab.,Hvd and water Resources. Ca1if.Inst.Tech, 1961. :46p.
(21)中国科学院地贡研究所,197数学地贡引论,地贡出版社,404页 |
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