[1] Longrman N W. Carbonate diagenetic textures from near surface diagenetic environment[J]. AAPG Bull. 1980,64:461~487
[2] 冯增昭等.中国沉积学[M].北京:石油工业出版社,1994.10.212~224
[3] Degens E T, Epstein S. Oxygen and carbon isotope ratios in coexisting calcites and dolomites from recent and ancient sediments[J]. Geochim. Cosmochim. Acta 1964,28: 23~ 44
[4] 冯增昭.华北地台早古生代岩相古地理研究[M].北京:地质出版社,1990.95~113
[5] 弗里德曼G M,桑德斯J E白云岩的成因及产状[M].冯增昭译.第一版.北京:石油工业出版社,1978.1~39
[6] Hsu K J, Siegenthaler C. Preliminary experiments on hydrodymmic movement induced by evaporation and their bearing on the dolomite problem[J]. Sedimentology, 1969,1~2:11 ~25
[7] Bathurst R G C. Carbonate sediments and their diagenesis, Developments in sedimentology[M]. Els. Publ. Com. 1971,12:1~ 7
[8] 福克RL,兰德LS.控制白云石结晶的两个因素:Mg/Ca比值和盐度[A]王尧译.国外地质.1977.10:105~136