Zircon U-Pb and Lu-Hf isotopic and geochemical constraints on the origin of the paragneisses from the Jiaobei terrane, North China Craton
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- 作者：Houxiang Shana ; b ; shanhouxiang@mail.iggcas.ac.cn" class="auth_mail" title="E-mail the corresponding author ; Mingguo Zhaia ; c ; Xiyan Zhuc ; M. Santoshd ; Tao Hongc ; Songsheng Gea ; b
- 关键词：Paragneisses ; Geochemistry ; Detrital zircon U&ndash ; Pb&ndash ; Hf isotopes ; Protolith ; Tectonic setting ; North China Craton
- 刊名：Journal of Asian Earth Sciences
- 出版年：2016
- 出版时间：1 January 2016
- 年：2016
- 卷：115
- 期：Complete
- 页码：214-227
- 全文大小：4867 K
文摘
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The protoliths of the paragneisses belong to clay–silty rocks and greywacke.
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The sediments of the protoliths were derived from an intermediate–acidic source.
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The Archean–early Paleoproterozoic granitic rock in Jiaobei was the major source.
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The protoliths of the paragneisses might have been deposited during 2.47–2.42 Ga.
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The protoliths of the paragneisses were deposited in a convergent margin setting.