{"title":"凯尔别斯-佐洛托基茨基矿群砂金来源的地球物理标志","authors":"P. Osipova, V. Olenchenko, V. Samorukov","doi":"10.3997/2214-4609.202152020","DOIUrl":null,"url":null,"abstract":"Summary The paper presents the capabilities of the electrical resistivity tomography for determining the thickness of loose sediments and the topography of an alluvial placer bedrock. Particular attention pays to identifying induced polarization anomalies associated with zones of gold-sulfide mineralization in bedrocks. These zones are the primary sources of placer gold in the region.","PeriodicalId":383927,"journal":{"name":"Engineering and Mining Geophysics 2021","volume":"4 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2021-04-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Geophysical Signs of Placer Gold’s Sources in Kelbes-Zolotokitatsky Ore-Placer Cluster\",\"authors\":\"P. Osipova, V. Olenchenko, V. Samorukov\",\"doi\":\"10.3997/2214-4609.202152020\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Summary The paper presents the capabilities of the electrical resistivity tomography for determining the thickness of loose sediments and the topography of an alluvial placer bedrock. Particular attention pays to identifying induced polarization anomalies associated with zones of gold-sulfide mineralization in bedrocks. These zones are the primary sources of placer gold in the region.\",\"PeriodicalId\":383927,\"journal\":{\"name\":\"Engineering and Mining Geophysics 2021\",\"volume\":\"4 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2021-04-26\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Engineering and Mining Geophysics 2021\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.3997/2214-4609.202152020\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Engineering and Mining Geophysics 2021","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.3997/2214-4609.202152020","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Geophysical Signs of Placer Gold’s Sources in Kelbes-Zolotokitatsky Ore-Placer Cluster
Summary The paper presents the capabilities of the electrical resistivity tomography for determining the thickness of loose sediments and the topography of an alluvial placer bedrock. Particular attention pays to identifying induced polarization anomalies associated with zones of gold-sulfide mineralization in bedrocks. These zones are the primary sources of placer gold in the region.
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