{"title":"高尔泰特列茨科湖滨带上奥陶统碳酸盐相特征","authors":"N. Sennikov, I. G. Zakiryanov, I. V. Varaksina","doi":"10.33764/2618-981x-2022-2-1-216-222","DOIUrl":null,"url":null,"abstract":"The large spherical structures found in the Upper Ordovician carbonates of the Teletskoe Lakeside structural-facies zone of the Gorny Altai were formed by algae. Oncolites-rhodolithes are indicators of shallow-water environments formed in the conditions with active hydrodynamics.","PeriodicalId":13672,"journal":{"name":"Interexpo GEO-Siberia","volume":"29 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2022-05-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Peculiarities of the Upper Ordovician carbonate facies of the Teletskoe Lakeside Zone, Gorny Altai\",\"authors\":\"N. Sennikov, I. G. Zakiryanov, I. V. Varaksina\",\"doi\":\"10.33764/2618-981x-2022-2-1-216-222\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"The large spherical structures found in the Upper Ordovician carbonates of the Teletskoe Lakeside structural-facies zone of the Gorny Altai were formed by algae. Oncolites-rhodolithes are indicators of shallow-water environments formed in the conditions with active hydrodynamics.\",\"PeriodicalId\":13672,\"journal\":{\"name\":\"Interexpo GEO-Siberia\",\"volume\":\"29 1\",\"pages\":\"\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2022-05-18\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Interexpo GEO-Siberia\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.33764/2618-981x-2022-2-1-216-222\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Interexpo GEO-Siberia","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.33764/2618-981x-2022-2-1-216-222","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Peculiarities of the Upper Ordovician carbonate facies of the Teletskoe Lakeside Zone, Gorny Altai
The large spherical structures found in the Upper Ordovician carbonates of the Teletskoe Lakeside structural-facies zone of the Gorny Altai were formed by algae. Oncolites-rhodolithes are indicators of shallow-water environments formed in the conditions with active hydrodynamics.
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