[1] (1)王国忠、吕炳全、全松青，1982,海南岛更新世白云羚的发现及其形成环垅分析，同济大学学报，4期，P .18-26。

(2)中国科学院南海海洋研究所地质研究宝，1978，华南沿海第四纪地质，科学出版社。

(3)杜恒俭、陈华慧、曹伯勋，1981，地貌学及第四纪地质学，地质出版社。

(4)北京农业大学编，1961,植物生理学(上、下)农业出版社。

(5)冯增昭，1979，白云岩的生成机理与成因分类，天然气勘探与开发，2期，P. 1一9。

(6)Folk。R. L.and Ward, W. C.，1975, Brazos river bar: A study in the sig-nification of grain size parameters, J. Sediment. Petrol. 27, p. 3-27.

(7)Warne, S.，1963, The Nature and Significance of Microscopic Mineral Matter in Some New South Wales Coals. Thesis, L,niv,New S. Wales, Sydney，N, S.W. 306 pp. Unpublished.

(8)Friedmaa，G. M. 1978, Staining Techniques, in Fairbridge, R. W. and Bour-geois, J. ed. The Encyclopedia of Sedimentology，Dowden，Hutchison and Ross,Inc, p. 764-765.

(9)Joint Commitee on Powder Diffraction Standards: Po+-der Diffraction File Set1-22(ASTM-J-JCPDS)。

(10)Chilingar, G. V'.，1957, Classification of Limestones and Dolomites on Basis of Ca/Mg Ratio. J. Sediment, Petrol.V.27. 187-189,

(11)Bathurst, R, G. C.，1971，Carbonate Sediments and their Diagenesis, Elsevier Publishing Company Amsterdam London Mew fork。

(12)Milliman, J, D, 1974, Marine Carbonates. Springar-Verlag Berlin. Heidelberg. New York.

(13)Friedman, G. M, and Sanders, J, E, 1967, Origin and Occurrence of dolomite， In: Chilingar, G. V.，et al.(Editors)，Carbonate Rocks,( Developments in Sedimentology，9A)Elsevier Publishing Company Amsterdam London New York.

(14) F olk，R, L. and Land, L, S.，1975, Mg/Ca ratio and Salinity;two Controls over Crystallization of Dolomite. Am. Assoc, Petroleum Geologists Bull, Vol. 59, p. 62-68,

(15) Liebermann, O., 1967, Synthesis of Dolomite, Nature 213: p. 241-245,

(16) Badiozamani，K,，1973, The Dolomitization Model-Application to the Middle Ordovician of Vdisconsin, J, Sediment. Petrol. Vol. 43, No, 4, p. 965-984.

(17)Hsu, K .J. and Siegenthaler, C.，1969, Preliminary experiments on hydrody- namic movement induced dy evaporation and their bearing on the dolomite problem, Sedimentology，12;11-25.