{"title":"花岗岩的起源","authors":"M. Okrusch, H. Frimmel","doi":"10.1130/mem28","DOIUrl":null,"url":null,"abstract":"Together with granodiorite and tonalite, granite constitutes the most common plutonic rock, collectively referred to as granitoids. Experimental studies on the simplified model system Qz–Or–Ab(–An)–H2O(–CO2) have shown that granitic magmas form by partial melting (anatexis) of the Earth’s lower crust.","PeriodicalId":234021,"journal":{"name":"Springer Textbooks in Earth Sciences, Geography and Environment","volume":"8 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"The Origin of Granite\",\"authors\":\"M. Okrusch, H. Frimmel\",\"doi\":\"10.1130/mem28\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Together with granodiorite and tonalite, granite constitutes the most common plutonic rock, collectively referred to as granitoids. Experimental studies on the simplified model system Qz–Or–Ab(–An)–H2O(–CO2) have shown that granitic magmas form by partial melting (anatexis) of the Earth’s lower crust.\",\"PeriodicalId\":234021,\"journal\":{\"name\":\"Springer Textbooks in Earth Sciences, Geography and Environment\",\"volume\":\"8 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\":\"Springer Textbooks in Earth Sciences, Geography and Environment\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1130/mem28\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Springer Textbooks in Earth Sciences, Geography and Environment","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1130/mem28","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Together with granodiorite and tonalite, granite constitutes the most common plutonic rock, collectively referred to as granitoids. Experimental studies on the simplified model system Qz–Or–Ab(–An)–H2O(–CO2) have shown that granitic magmas form by partial melting (anatexis) of the Earth’s lower crust.
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