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扬子克拉通北缘米仓山地区基底变质岩系同位素地质年代学
ISOTOPIC GEOCHRONOLOGY OF BASEMENT METAMORPHIC ROCK SERIES IN THE MICANGSHAN AREA ALONG THE NORTHERN MARGIN OF YANGTZE CRATON,CHINA
【摘要】 单锆石铅同位素蒸发法年龄研究表明,扬子克拉通北缘米仓山地区基底变质岩系中后河岩群形成于晚太古宙—早元古宙,火地垭群形成于中上元古宙;之后在晋宁运动晚期和澄江期各发生了一次大规模的构造热事件。
【Abstract】 It is assumed that the age of the Houhe rockgroup is Late Archean to Early Protorozoic and that the age of the Huodiya Group is MesoNew Proterozoic in the metamorphic basement of the Northern margin of the Yangtze craton by the studying on the Pb isotopic geochronology of single zircon.It is substaintiated that there were two very important tectonothermal events at Late Jinningian and Chengjianggian respectively.
- 【文献出处】 矿物岩石 ,JOURNAL OF MINERALOGY AND PETROLOGY , 编辑部邮箱 ,1997年S1期
- 【分类号】P597.3
- 【被引频次】25
- 【下载频次】301