[1] |
1 大港油田研究所等,1985,滦河冲积扇一三角洲沉积体系,北京:地质出版社。 2 任明达、李淑莺等.1988.渤海现代海进现象剖析,海洋学报,1期,67-75页。 3 昊秀杰、田素珍等,1986,河北海岸带波浪状况分析,黄渤海海洋,3期,9-15页。 4 昊正,1987,风沙地貌学,北京:科学出版社。 5 高善明,1983.滦河口北岸海岸沙丘的形成时代,海洋湖沼通报,3期,30-32页。 6 蔡爱智、蔡月娥,1983,中国海岸风沙沉积的形成与特征,中国沙漠.3期.1-10页。 7 Bagnold R.A.,1941,The Physics of Blown Sand and Desert Dunes. Methuen&Co. Ltd.,London. p.56一183. Cooper W: S.,1958. Coastal Sand Dune of Gregon and Washington. Geol. Society of America Memoir 72, p. 169. 8 Gornitz V.S.,1982. Global sea levee trend in the past century. Science, V. 215, p. 1161一1614. 9 Hunter R. H. and Richmond B. M.,1988. Daily clycles in the coastal dunes. Sediment. Geol.,V.55, p.43一67. 10 Pye K. and Bowman G. M.,1984, The Holocence marine transgression as a forcing function in episodic dune activity on eastern Australian coast. In:Thom B. G. (ed.),Coastal Geomorphology in Australia. Academics Press,Sydney.p. 179一186. 11 Short A. D. and Hesp P. A.,1982. Wave, beach and dune interactions in Southeastern Australia. Marine Geol.,V.48. p.259一284. 12 Wright L. D. et al.,1979. Morphodynamics of reflective and dissipative beach and inshore systems,Southeastern Australi-a. Marine Geol.,V. 32, p. 105一140. |