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在借助新技术了解碳酸盐岩的沉积和成岩作用方面取得的新进展,包括有关白云岩化的新概念。白云岩质沉积物在蒸发环境中的发现,使得一些研究者相信大多数白云岩是燕发成因的。然而,伴生蒸发岩及有关干化特点的缺失使这一通用的概念得到了修正。 60年代末期,H.G.Goodell和R.K.Garman(1969)提出降水可能对白云岩的形成有影响。后来,Hanshaw,Back和Deike(1971),L.S.Land(1973),K.Badiozani(1973),R.L.Folk和
New advances in understanding carbonate sedimentation and diagenesis with new technologies include a new concept of dolomitization. The discovery of dolomitic sediments in an evaporative environment has led some researchers to believe that most dolomites are caused by trash. However, the absence of associated evaporites and related features of drying has led to the revision of this general concept. In the late 1960s, H. G. Goodell and R.K. Garman (1969) suggested that precipitation may have an impact on dolomite formation. Later, Hanshaw, Back and Deike (1971), L. S. Land (1973), K. Badiozani (1973), R. L. Folk and