【摘要】 淡水湖泊在咸化为盐湖或碱湖过程中必然经历湖相碳酸盐岩沉积阶段，但至今在国内、外湖相碳酸盐岩研究仍处于湖泊沉积学研究的极薄弱领域。我国第三系古湖泊具有不同的演化方向，大多数问盐湖演化（沉积盐岩）[1]，泌阳凹陷则不同，它向苏打湖演化（沉积碱岩），因而将泌阳凹陷作为向苏打湖演化的典型代表加以剖析，对于对比研究不同类型湖泊中湖相碳酸盐（岩）发育特征和建立沉积模式不仅具有重要的理论意义，而且对评价油气潜能和指导油气勘探也十分有意义。更多还原

【Abstract】 Being one of the most important oil source rock in Biyang depression,the Iacustrine carbonate rock is,here,mainly composed of dolomite, representing the characteristics of lacustrine carbonate rocks formed ln the course of soda lake evolution Under the hot and semi-arid paleoclimate, the upper and lower part of the lower Tertiary are coarse clastic rocks which formed fluvial and Lacustrine facies in interval. The middle part Hetaoyuan Formation consists mainly of lacustrine muddy shale,carbonate and alkaline rocks except fan delta and delta deposits.The depositional model of lacustrine carhonate rocks evoluted to the soda lake: (1)The fan delta facies and delta facies are distributed along the south and north margin of the depression respectively,for the abundant supplement of clastics and low salinity (3‰- 6‰,)are generally not favorable for the formation of carbonate deposition, only forming lots of authigenic calcite and little authigenic dolomite minerals dispersing in mudstone and sandstone or the cements of sandstones. Particularly,in delta facies during flood-interval period or in interchannel deposits,the authigenic ferrodolomite and lime mudstone sheet increases with some lime mud shell oolites, intraclast sandstone and cryptoalgal laminated rocks intercalation deposited; (2)The salinity of lake water ln Lake-shore and lakeubay facies,especially in the latter is high, the authigenic calcites and lime mudstone, ferrodolostone are widespread, in these facies, meanwhile, true ooid-and superficial ooid-bearing grain carbonate rock increases as well; (3)Carbonate rocks in shallow Lake facies are well doveloped,and the total thickness of carbonate rocks is about 300-600 m. The lithology are mainly grey -black, brown -grey dolomite mudstone, ferrodolostone and ooid - intraclast -bearing dololnite mudstone exceljt alkalinebearing lumps and lime mudstone deposition in the near-shore shollow lake facies; (4)Deeper lake facies, excluding turbidite deposition,are short of supplement of fresh water and clastics in deeper water depth and stable depositional environment. The salinity of lake water is hlgh. Dolomite mudstone deposition is the thickest and about 700-900 m. The lithology are mainly black, grey-black dolomite mudstone, ferrodolostone and dolomitic muddy shale lamllar interbedded. These are the typical characteristics of lacustrine carbonate-type oil source rock. Nowadays, the oil field has been found here ; (5)The salinity of alkaline lake facies is very high (30%,‰-60‰), all kinds of carbonate rock, especially lime mudstone and ferrocalcite rock, are well developed and lamellar interbedded with alkaline layers and clastic rocks. Carbonate rocks formed excellent evaporitebearing carbonate-type oil source rock.更多还原