{"title":"外贝加尔湖西部软玉的液体来源","authors":"M. Rampilova, G. Ripp, M. Rampilov","doi":"10.31554/978-5-7925-0584-1-2020-371-374","DOIUrl":null,"url":null,"abstract":": isotope data of apocarbonate nephrites of the Vitim nephrite-bearing area are given. They haveonly mete-oric-derived water source. Granites which concidered the source of water fluids produce only recycling of these waters. The oxygen in calciphyre was used from the altered matrix and formation water.","PeriodicalId":208191,"journal":{"name":"WATER-ROCK INTERACTION: GEOLOGICAL EVOLUTION","volume":"32 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"SOURCES OF FLUIDS APOCARBONATE NEPHRITES OF WESTERN TRANSBAIKALIA\",\"authors\":\"M. Rampilova, G. Ripp, M. Rampilov\",\"doi\":\"10.31554/978-5-7925-0584-1-2020-371-374\",\"DOIUrl\":null,\"url\":null,\"abstract\":\": isotope data of apocarbonate nephrites of the Vitim nephrite-bearing area are given. They haveonly mete-oric-derived water source. Granites which concidered the source of water fluids produce only recycling of these waters. The oxygen in calciphyre was used from the altered matrix and formation water.\",\"PeriodicalId\":208191,\"journal\":{\"name\":\"WATER-ROCK INTERACTION: GEOLOGICAL EVOLUTION\",\"volume\":\"32 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1900-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"WATER-ROCK INTERACTION: GEOLOGICAL EVOLUTION\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.31554/978-5-7925-0584-1-2020-371-374\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"WATER-ROCK INTERACTION: GEOLOGICAL EVOLUTION","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.31554/978-5-7925-0584-1-2020-371-374","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
SOURCES OF FLUIDS APOCARBONATE NEPHRITES OF WESTERN TRANSBAIKALIA
: isotope data of apocarbonate nephrites of the Vitim nephrite-bearing area are given. They haveonly mete-oric-derived water source. Granites which concidered the source of water fluids produce only recycling of these waters. The oxygen in calciphyre was used from the altered matrix and formation water.
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