{"title":"硅酸盐熔体硫化物饱和度的热力学控制及其在海底玄武岩中的应用。","authors":"H. O’Neill","doi":"10.1002/essoar.10503096.1","DOIUrl":null,"url":null,"abstract":"A thermodynamic model to calculate the “Sulfide Content at Sulfide Saturation” or SCSS of basaltic and intermediate composition silicate melts has been built from four independently measurable ther...","PeriodicalId":202445,"journal":{"name":"Magma Redox Geochemistry","volume":"19 3","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2020-05-14","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"23","resultStr":"{\"title\":\"The thermodynamic controls on sulfide saturation in silicate melts with application to Ocean Floor Basalts.\",\"authors\":\"H. O’Neill\",\"doi\":\"10.1002/essoar.10503096.1\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"A thermodynamic model to calculate the “Sulfide Content at Sulfide Saturation” or SCSS of basaltic and intermediate composition silicate melts has been built from four independently measurable ther...\",\"PeriodicalId\":202445,\"journal\":{\"name\":\"Magma Redox Geochemistry\",\"volume\":\"19 3\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2020-05-14\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"23\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Magma Redox Geochemistry\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1002/essoar.10503096.1\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Magma Redox Geochemistry","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1002/essoar.10503096.1","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
The thermodynamic controls on sulfide saturation in silicate melts with application to Ocean Floor Basalts.
A thermodynamic model to calculate the “Sulfide Content at Sulfide Saturation” or SCSS of basaltic and intermediate composition silicate melts has been built from four independently measurable ther...