极地乌拉尔地区Ray-Iz蛇绿岩铬铁矿中的钻石和高还原矿物:足状铬铁矿和蛇绿岩钻石的深层成因

{"title":"极地乌拉尔地区Ray-Iz蛇绿岩铬铁矿中的钻石和高还原矿物:足状铬铁矿和蛇绿岩钻石的深层成因","authors":"J. Yang, R. Wirth, M. Wiedenbeck, W. Griffin, F. Meng, S. Y. Chen, W. Bai, X. Xu, A. B. Makeeyev, N. I. Bryanchaniniova","doi":"10.1111/1755-6724.12308_64","DOIUrl":null,"url":null,"abstract":"","PeriodicalId":179830,"journal":{"name":"Acta Geological Sinica","volume":"9 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2015-12-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Diamonds and highly reduced minerals from chromitite of the Ray-Iz ophiolite of the Polar Urals: deep origin of podiform chromitites and ophiolitic diamonds\",\"authors\":\"J. Yang, R. Wirth, M. Wiedenbeck, W. Griffin, F. Meng, S. Y. Chen, W. Bai, X. Xu, A. B. Makeeyev, N. I. Bryanchaniniova\",\"doi\":\"10.1111/1755-6724.12308_64\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"\",\"PeriodicalId\":179830,\"journal\":{\"name\":\"Acta Geological Sinica\",\"volume\":\"9 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2015-12-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Acta Geological Sinica\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1111/1755-6724.12308_64\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Acta Geological Sinica","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1111/1755-6724.12308_64","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}