Source and mode of the Permian Panjal Trap magmatism: Evidence from zircon U-Pb and Hf isotopes and trace element data from the Himalayan ultrahigh-pressure rocks
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- 作者：Hafiz Ur Rehmana ; hafiz@sci.kagoshima-u.ac.jp" class="auth_mail" title="E-mail the corresponding author ; Hao-Yang Leeb ; c ; Sun-Lin Chungb ; c ; Tahseenullah Khand ; Patrick J. O'Briene ; Hiroshi Yamamotoa
- 关键词：Himalaya ; Panjal Traps ; UHP eclogites and felsic gneisses ; Zircon U&ndash ; Pb age ; Hf isotopes ; Trace element geochemistry
- 刊名：Lithos
- 出版年：2016
- 出版时间：1 September 2016
- 年：2016
- 卷：260
- 期：Complete
- 页码：286-299
- 全文大小：3652 K
文摘
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Himalayan UHP eclogites and some of the surrounding felsic gneisses were produced during the Permian Panjal Trap magmatism.
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The Panjal Trap magmatism was bimodal.
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U–Pb age and Hf isotope data from zircons indicate juvenile mantle source for the protoliths of eclogites and felsic gneisses.
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