[1] 赵希涛等,1979,地质科学,4期,342-3580
[2] 赵希涛等,1978,地质科学,2期,163-1730
[3] 沙庆安等,1981,西沙群岛和海南岛现代和全新世海相碳酸盐的成岩作用—兼谈海相表成(海相淡成)灰岩及其意义,沉积岩学研究(论文集),科学出版社。
[4] 张景文等,1981,地震地质,3卷1期,6。
[5] 王国忠,吕炳全,1984,沉积学报,2卷1期,18-280
[6] Friedman, G.M.,Amiel, A.J.and Schneidermann, N.,1974, SubmarineCementation in Reefs,Example from The Red Sea, Jour.Sed. Petrology,V. 44, P.816一825.
[7] lames, N. P. et al.,1976, Facies and Fabric Specificity of Early Sub-sea Cements in Shallow Belize(British Honduras)Reefs:lour. Sed.Petro-logy, V.46, P. 523一544.
[8] Alexandersson, T.,1972, Intragranular Growth of Marine Aragonite and Mg一calcite: Evidence of Precipitation from Supersaturated Sea Water, Jour. Sed.petrology, V. 42, P.441一460.
[9] Longman, M.W.,1980, Carbonate Diagenetic Textures fro m Near Sur-face Diagenetic Enviroments, Am.Assoc. Ptrol.Geolgists Bull.,V.64, P. 461一487.
[10] Chilingar, G. V. et al, 1979, Diagenesis of Carbonate Sediments and Epigen-esis(or Catagenesis)of Limestones,In: Diagenesis in Sediments and Sedimentary Rocks(G. V. Chilingar Ed.),247一424, Elsevier S cientific Publishing Co.,Amsterdan一Oxford一New York.