[1] (1)陈以健，焦文强，1982，西沙群岛石岛的放射性碳剖面:近代地壳运动的证据，《海洋地质研究》第二卷第二期

(2)廖士范，1981，我国广东海南岛、西沙群岛现代碳酸盐岩的地质时代及有关成岩阶段，贵州地质科技情报，第三期。

(3)王国忠、吕炳全，1981，西沙群岛石岛上沉积背斜等组构的指相意义，同济大学学报，第四 期。

(4)业治铮、张明书等，1984，西沙石岛风成石灰岩和化石土壤的发现及其意义，海洋地质与第四纪地质，第四卷第一期。

(5)Mckee E.D. 1966a, Structures of dunes at White Sands National Monument,New Misico (and a composition with structures of dunes from other selectedareas) "Sedimentology" vol.7, p,1-69

(6)Mckee E.D. 1982, Sedimentary structure=s in dunes of the Namib Desert, South Africa. Geol.Soc.Am.Special paper 188.

(7)Mainguest, Monique and Callot 1974, Air photo study of topology and interre- actions between the tezture and structure of dune patterns in the Fachi-Bilma Erg, Sahara.

(8)Walker R.G.and Middleton G. V.1979, Eacies ModelsGeosci.Can.4.

(9)Stokes S.L. 1968, Multiple parallel truncation bedding wind deposited sandstone formations J .Sedim.Petrol.vol. 38.p 510-515.

(10) Brookfield M. E. 1977, The origin of boundary surfaces dstones

plane features of in ancient aeolian san-dstones Sedimentology vol. 24. 303-332.

(11) Kocurek G.1981, Significance of interdune deposits and bounding surfaces in aeolian dune sandsSedimentology vol.28 p 753-780.

(12) Walker T. R.and J.C.Harms 1972, Eolian origin of flagstone beds, Lyons sandstone (Permian)，type area, B oulder C ounty，Colorado Mountain Geol.vol。9 .278-288.

(13)Fairbridge R.W. and Teichert C. 1953, Soil horizons and marine bands in the coastal limestones of Western Australia J .Roy.Soc N.S.Wales vol.86 .68-87

(14)Curray J.R.1965, Late Quaternary History，Continental Shelves of the Uni-ted States, In Wright, H.E.Jr.et al.(eds.)The Quaternary of the United States, Princeton U niv.Press, .723-735.