在碳酸盐地层中的油、气藏(田)和凝析气藏(田)中,大多数属于层状碳酸盐地层(即有别于不成层的礁和残山的碳酸盐地层——译注)。马克西莫维奇将它们划分为局部具孔洞的碳酸盐岩地层和区域性具孔洞的碳酸盐岩地层两种(1973)。新获得的资料说明,在这两种储集层中,除了主要有孔洞外,其他如大洞、淋 Most of the oil, gas reservoirs (fields) and condensate gas fields (fields) in carbonate formations belong to stratiform carbonate formations (ie, carbonate strata distinct from stratigraphic reefs and residual hills - Annotation). Maximovitch divides them into two types of locally porous carbonate beds and regional porous carbonate beds (1973). The newly obtained information shows that in both reservoirs, in addition to the major holes, others such as large holes and leaching