ASSESSMENT OF INFLUENCE OF PALEOGEOGRAPHICAL CONDITIONS ON THE FORMATION OF MINERAL RAW MATERIALS FOR THE MANUFACTURE OF CERAMIC PRODUCTS (ON THE EXAMPLE OF OPISHNYANSKE DEPOSIT OF CLAY ROCKS)
{"title":"ASSESSMENT OF INFLUENCE OF PALEOGEOGRAPHICAL CONDITIONS ON THE FORMATION OF MINERAL RAW MATERIALS FOR THE MANUFACTURE OF CERAMIC PRODUCTS (ON THE EXAMPLE OF OPISHNYANSKE DEPOSIT OF CLAY ROCKS)","authors":"Zh.M. Matviishyna, S. Doroshkevych, A. Kushnir","doi":"10.15407/UGZ2021.01.015","DOIUrl":null,"url":null,"abstract":"The main properties and features of clay rocks, which are the basic raw materials for the manufacture of ceramic products are outlined. The main morphogenetic, physicochemical and geochronological characteristics of clay rocks of the Opishnyanske deposits (Poltava region) are covered, the natural conditions of this mineral raw material formation in the late Miocene, Pliocene and Pleistocene are reconstructed, the role of paleogeographic conditions in their formation and accumulation is estimated. Perspective locations of their place position are marked out basing on paleogeographical data.","PeriodicalId":36917,"journal":{"name":"Ukrainian Geographical Journal","volume":"36 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2021-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Ukrainian Geographical Journal","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.15407/UGZ2021.01.015","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"Arts and Humanities","Score":null,"Total":0}
引用次数: 1
Abstract
The main properties and features of clay rocks, which are the basic raw materials for the manufacture of ceramic products are outlined. The main morphogenetic, physicochemical and geochronological characteristics of clay rocks of the Opishnyanske deposits (Poltava region) are covered, the natural conditions of this mineral raw material formation in the late Miocene, Pliocene and Pleistocene are reconstructed, the role of paleogeographic conditions in their formation and accumulation is estimated. Perspective locations of their place position are marked out basing on paleogeographical data.