[1] Off T. Rhythmic linear sand bodies caused by tidal currents. Bulletin of AAPG, 1963,47(2):324-341. [2] Caston V N D, Stride A H. Tidals and movement between some linear sand banks in the North Sea off northeast Norfolk.Marine Geology,1970,9:M38-M42. [3] Caston G F. Potential gain and loss of sand by some sand banks in the southern North Sea off northeast Norfolk. Marine Geology,1981,41:239-250. [4] Swift D J P. Tidal sand ridges and shoal-retreat massifts. Marine Geology, 1975, 18:105-134. [5] Swift D J P, Field M E. Evolution of a classic sand ridges field: Maryland sector,North American inner shelf. Sedimentology, 1981, 28:461-482. [6] Amos G L, King E L. Bedforms of the Canadian Eastern seaboard: a comparison with global occurrences. Marine Geology, 1984, 57:167-208. [7] Parker G, Lanfredi N W , Swift D J P. Seafloor response to flow in southern Hemisphere and ridge field: A rgentine Inner shelf. Sedimentary Geology, 1982, 33:195-216. [8] Harris P T,Pattiaratchi C B,Cole A R,et al. Evolution of subtidal sandbanks in Moreton Bay,eastern Australia.Marine Geology, 1992, 103: 225-247. [9] 刘振夏, 夏东兴. 潮流脊的初步研究. 海洋与湖沼, 1983, 14(3): 286-295. [10] 夏东兴, 刘振夏. 潮流脊的形成机制和发育条件. 海洋学报, 1984, 6(3): 361-367. [11] 汤毓祥, 姚兰芳, 刘振夏. 辽东浅滩海域潮流运动特征及其与潮流脊发育的关系. 黄渤海海洋, 1993, 11(4), 9-16. [12] 汤毓祥, 刘振夏, 姚兰芳. 渤海M2潮流及其与辽东浅滩潮流脊发育的关系. 海洋通报, 1994, 13(1): 25-29. [13] 刘振夏, 夏东兴, 汤毓祥, 等. 渤海东部全新世潮流沉积体系. 中国科学(B辑), 1994,24(12):1331-1338. [14] 刘振夏, 夏东兴. 潮流沙脊的水力学问题探讨. 黄渤海海洋, 1995, 13(4): 23-28. [15] 刘振夏. 中国陆架潮流沉积研究新进展. 地球科学进展, 1996, 11(4): 414-416. [16] Houbolt J J H C. Recent sediment in the southern bight of the North Sea. Geologie Mijnbouw, 1968, 47:245-273. [17] Swift D J P, Duane D B, Mckinney T F. Ridge and swale topography of the middle Atlantic Bight, north America. Marine Geology, 1973, 15:227-247. [18] McCave I N. Tidal currents at the North Hinder light ship, southern North Sea: Flow direct ions and tubulence in relation to maintenance of sand banks. Marine Geology, 1979, 31:101-117. [19] Soulsby R L. Measurements of the Reynolds stress components close to a marine sandbanks. Marine Geology, 1981, 31:101-114. [20] Howarth M J, Huthnance J M. Tidal and residual circulation around a Norfolk sandbank. Esturarine and Coastal Shelf Science, 1984, 19:105-117. [21] Smith J D. Geomorphology of a sand ridge. Journal of Geology, 1969, 77: 39-55. [22] Belderson R H, Johnson M A, Kenyon N H. Bedforms. In: Stride A H, ed. Offshore tidal sands: processes and deposits. London: Chapman and Hall, 1982. 27-57. [23] Johns B. Physical oceanography of coastal and shelf seas . New York: Elsevier, 1983. 321-386. [24] Huthnance J M. On one mechanism forming linear sandbanks. Estuarine and Coastal Shelf Science, 1982a, 14:79-99. [25] Huthnance J M. On the formation of sandbanks of finite extent. Estuarine and Coastal Shelf Science, 1982b, 15:277-299. [26] Pattiaratchi C B, Collins M B. Mechanisms for linear sandbank formation and maintenance in relation to dynamical oceanographic observations. Prog Oceanog, 1987,19:117-176. [27] Collins M B, Shimwell S J, Gao S,et al.Water and sediment movement in the vicinity of linear sandbanks:the Norfolk Banks, Southern North Sea. Marine Geology, 1995, 123:125-142. [28] 刘振夏, 汤毓祥, 王揆洋, 等. 渤海东部潮流动力地貌特征. 黄渤海海洋, 1996, 14(1): 7-20. [29] 方国洪, 杨景飞. 渤海潮运动的一个二维数值模型. 海洋与湖沼, 1985, 16(5): 337-345. |