{"title":"东欧地台的深经向构造","authors":"Viktor A. Ogadzhanov","doi":"10.18500/1819-7663-2022-22-3-185-190","DOIUrl":null,"url":null,"abstract":"Using a complex of remote and surface geophysical methods in the eastern part of the East European Platform, regional meridional heterogeneitieswere revealed; it isshown that these heterogeneitiescan becaused by low-density and magnetically active rocks in thecrystalline crust and mantle. The totality of geological and geophysical data indicates the relationship of meridional heterogeneities with transcontinental deep faults.","PeriodicalId":193038,"journal":{"name":"Izvestiya of Saratov University. Earth Sciences","volume":"34 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2022-08-24","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Deep meridional structures of the East-European platform\",\"authors\":\"Viktor A. Ogadzhanov\",\"doi\":\"10.18500/1819-7663-2022-22-3-185-190\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Using a complex of remote and surface geophysical methods in the eastern part of the East European Platform, regional meridional heterogeneitieswere revealed; it isshown that these heterogeneitiescan becaused by low-density and magnetically active rocks in thecrystalline crust and mantle. The totality of geological and geophysical data indicates the relationship of meridional heterogeneities with transcontinental deep faults.\",\"PeriodicalId\":193038,\"journal\":{\"name\":\"Izvestiya of Saratov University. Earth Sciences\",\"volume\":\"34 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2022-08-24\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Izvestiya of Saratov University. Earth Sciences\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.18500/1819-7663-2022-22-3-185-190\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Izvestiya of Saratov University. Earth Sciences","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.18500/1819-7663-2022-22-3-185-190","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Deep meridional structures of the East-European platform
Using a complex of remote and surface geophysical methods in the eastern part of the East European Platform, regional meridional heterogeneitieswere revealed; it isshown that these heterogeneitiescan becaused by low-density and magnetically active rocks in thecrystalline crust and mantle. The totality of geological and geophysical data indicates the relationship of meridional heterogeneities with transcontinental deep faults.
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