The new Evidence of Southward Subduction of the Middle Tethys Oceanic Basin in the Weat Segment of Bangonghu-Nujiang Suture, Tibet, Nawucuo area:Zircon U-Pb LAICPMS Dating and Lithogeochemistry of arc Granites | |
HU Jun; WAN Yongwen; ZHANG Dan | |
2013 | |
会议日期 | 2013-6-17 |
会议地点 | 成都 |
关键词 | Tibet plateau arc granite rocks zircon U-Pb LA-ICPMS dating Bangonghu-Nujiang suture |
会议录 | The First Joint Scientific Meeting of Geological Society of China and Geological Society of America(roof of the world)(第一届中国地质学会与美国地质学会联合学术会议——世界屋脊讨论会)论文集
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URL标识 | 查看原文 |
内容类型 | 会议论文 |
URI标识 | http://www.corc.org.cn/handle/1471x/4676750 |
专题 | 成都理工大学 |
作者单位 | [1]Chengdu University of Technology,Erxian bridge east three road 1#,Chengdu,Sichuan,610059,China |
推荐引用方式 GB/T 7714 | HU Jun,WAN Yongwen,ZHANG Dan. The new Evidence of Southward Subduction of the Middle Tethys Oceanic Basin in the Weat Segment of Bangonghu-Nujiang Suture, Tibet, Nawucuo area:Zircon U-Pb LAICPMS Dating and Lithogeochemistry of arc Granites[C]. 见:. 成都. 2013-6-17. |
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