海岸沙洲

海岸沙洲是指沿海岸线分布的宽阔沙带，其表面呈现出界限分明的平行或半平行沙脊，沙脊之间由浅洼地隔开。海岸沙洲通常是由波浪和沿岸流将河口两侧的粗沉积物重新堆積而形成的。McCubbin, D.G., 1982, Barrier-island and strand-plain facies. in P.A. Scholle, and D. Spearing, eds., pp. 247–279., Sandstone Depositional Environments: Memoir no. 31, Tulsa, Oklahoma, American Association of Petroleum Geologists, Tulsa, Oklahoma.Fitzgerald, D.M., W.J. Cleary, I.V. Buynevich, C.J. Hein, A.H.F. Klein, N. Asp, and R. Angulo, 2007, Strandplain Evolution along the Southern Coast of Santa Catarina, Brazil. Journal of Coastal Research. Supplemental issue no. 50, pp. 152-156.

参考文献

Category:海岸及海洋地形