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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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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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