{"title":"副锆石晶体孪晶的显微显示","authors":"Robert Sturm","doi":"10.1093/mictod/qaad071","DOIUrl":null,"url":null,"abstract":"Abstract In general, crystal twinning in accessory zircon represents a rare, but in almost all granites and gneisses, encounterable phenomenon. Since only the crystal face {101} occurs as a twin plane, formation of crystal twins turns out to be relatively simple. Besides geniculate twins, which develop by rotation of the crystal structure about the line [101], parallel twins that are arranged parallel to the crystallographic main axis of zircon can also be observed by light and electron microscopy. While geniculate twins usually show a frequency within the region of a permille, the number of parallel twins can rise to several percent depending on the investigated rock. In the present contribution, a brief insight into the microscopic world of zircon twinning is provided.","PeriodicalId":74194,"journal":{"name":"Microscopy today","volume":"131 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2023-09-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Microscopic Visualization of Crystal Twinning in Accessory Zircon\",\"authors\":\"Robert Sturm\",\"doi\":\"10.1093/mictod/qaad071\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Abstract In general, crystal twinning in accessory zircon represents a rare, but in almost all granites and gneisses, encounterable phenomenon. Since only the crystal face {101} occurs as a twin plane, formation of crystal twins turns out to be relatively simple. Besides geniculate twins, which develop by rotation of the crystal structure about the line [101], parallel twins that are arranged parallel to the crystallographic main axis of zircon can also be observed by light and electron microscopy. While geniculate twins usually show a frequency within the region of a permille, the number of parallel twins can rise to several percent depending on the investigated rock. In the present contribution, a brief insight into the microscopic world of zircon twinning is provided.\",\"PeriodicalId\":74194,\"journal\":{\"name\":\"Microscopy today\",\"volume\":\"131 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2023-09-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Microscopy today\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1093/mictod/qaad071\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Microscopy today","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1093/mictod/qaad071","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Microscopic Visualization of Crystal Twinning in Accessory Zircon
Abstract In general, crystal twinning in accessory zircon represents a rare, but in almost all granites and gneisses, encounterable phenomenon. Since only the crystal face {101} occurs as a twin plane, formation of crystal twins turns out to be relatively simple. Besides geniculate twins, which develop by rotation of the crystal structure about the line [101], parallel twins that are arranged parallel to the crystallographic main axis of zircon can also be observed by light and electron microscopy. While geniculate twins usually show a frequency within the region of a permille, the number of parallel twins can rise to several percent depending on the investigated rock. In the present contribution, a brief insight into the microscopic world of zircon twinning is provided.
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