[1] (1) Bloom A.L.,Broecl}r W.S.,Chappell J., Matthews R.K. and Mesolella, K.J.,1974, Quat.Res.. V.4. p.185-205.

(2) Hathutst R.G.C.. 1976, Carbonate Sediments and their Diagenesis.Elsevier. Amsterman, 658p

(3) ChappellJ., 1974, GeoLSoc.Amer.Bull.. V.85, p.553-570.

(4) Constqntz B.K., 1986, The primary surface area of corals and varuations in their susceptibility to diagenesis, In: Schroeder, J.H., and Purser, B.H. (eds), Reef Diagenesis, Springer-Ve}lag Berlin, p.p3-76.

(5) James N.P., 1974, J.Paleontol.. V.48, p.785-799.

(6) Longman M.W., 1980, A.A.P.G. Bull., V.64, p.461-487.

(7) Macintyre LG., 1976, J.Sed.Petrol.,V.47, p.503-Sib.

(8) Msrshall J.,1986, Regional distribution of submarine cements within an eqicontinental reef system: central Great Barrier Reef, Australia, In: Schroeder. J. H.,and ?urser, B. H.(eds),Reef Diagenesis. Springer-Verlag Berlin, p.8-26.

(9) Matthews R.K., 1968, J.Sed.Pdtrol., V.38, p.1110-1119.

(10) PingitoreN.E., 1976, J.Sed.Petrol., V.46, p.985-1006

(I1) Schlanger S.O., 1963, U.S.Geo!.Surv.Prof.Paper. 260 BB, p.991-1038.

(12) Schubert C.,1977, Pleistocene M arine terraces of La Alanyuila Island, Vet:czuela, and their diagenesis. Proc.3td Intern.Coral Reef 5ymp., V.2, Miami, p.149-154.

(13) Shinn E.A., 1969, Sedimentology, V.12, p.109-144.

(14) Tebbutt G.E.. 1975, AAPG Studies in Geo1.V.2, p.297-331.