{"title":"Hydrogeological Settings of Sediments of the Permo-triassic Complex of the Eastern Ciscaucasia","authors":"A. Saltanova, V. Yakushev","doi":"10.3997/2214-4609.201802365","DOIUrl":null,"url":null,"abstract":"The schematic maps of mineralization, metamorfization degree, sulfatation degree of the reservoir solutions and other parameters were constructed on the basis of the analysis of the reservoir solution samples which were taken from the deposits of the Permo-Triassic complex on the territory of the Eastern Ciscaucasia platform part. The distribution of three hydrogeochemical zones of the studied complex is revealed and traced. As a result of the comparative analysis of the Permian-Triassic hydrogeological complex with the above-lying sediments, the inverse nature of a hydrogeological section of the Eastern Ciscaucasia was established.","PeriodicalId":288128,"journal":{"name":"20th conference on oil and gas geological exploration and development","volume":"4 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2018-09-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"20th conference on oil and gas geological exploration and development","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.3997/2214-4609.201802365","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
The schematic maps of mineralization, metamorfization degree, sulfatation degree of the reservoir solutions and other parameters were constructed on the basis of the analysis of the reservoir solution samples which were taken from the deposits of the Permo-Triassic complex on the territory of the Eastern Ciscaucasia platform part. The distribution of three hydrogeochemical zones of the studied complex is revealed and traced. As a result of the comparative analysis of the Permian-Triassic hydrogeological complex with the above-lying sediments, the inverse nature of a hydrogeological section of the Eastern Ciscaucasia was established.