{"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.
求助内容：
应助结果提醒方式：
京公网安备 11010802042870号
