Abstract

Rocks in the Galitsyno quarry located in the Adler region of the North Caucasus are described. The quarry is of interest, because the excellent exposure in the relatively homogeneous carbonate rock sequence makes it possible to identify certain changes that reflect events that were common to the Late Cretaceous, in this case, the Late Campanian. These include the carbonate sedimentation characteristics of this geochronological interval, constant fluctuations in the relative sea level, and periodic volcanic activity. All these events are confirmed by the structural features of the section, various lithological rock types, as well as by the specific composition of microorganism complexes. The use of different methods in the analysis of the factual material makes these conclusions convincing.

中文翻译：

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西北高加索坎帕阶矿床构造及形成条件（Galitsyno剖面）

摘要

描述了位于北高加索阿德勒地区的 Galitsyno 采石场的岩石。该采石场很有趣，因为在相对均质的碳酸盐岩序列中的极好暴露使得可以识别反映晚白垩世（在本例中为晚坎帕阶）常见事件的某些变化。其中包括该地质年代间隔的碳酸盐沉积特征、相对海平面的持续波动以及周期性的火山活动。所有这些事件都被该剖面的结构特征、各种岩性岩石类型以及微生物复合体的特定组成所证实。在对事实材料的分析中使用不同的方法使这些结论具有说服力。