Geochemistry of Neoarchean (ca. 2.55-2.50 Ga) volcanic and ophiolitic rocks in the Wutaishan greenstone belt, central orogenic belt, North China craton: Implications for geodynamic setting and continental growth: Discussion

Guochun Zhao; Alfred Kr?ner

首页> 外文期刊>GSA Bulletin >Geochemistry of Neoarchean (ca. 2.55-2.50 Ga) volcanic and ophiolitic rocks in the Wutaishan greenstone belt, central orogenic belt, North China craton: Implications for geodynamic setting and continental growth: Discussion

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Geochemistry of Neoarchean (ca. 2.55-2.50 Ga) volcanic and ophiolitic rocks in the Wutaishan greenstone belt, central orogenic belt, North China craton: Implications for geodynamic setting and continental growth: Discussion

机译：中国北部克拉通五台山绿岩带，中部造山带的新太古代（约2.55-2.50 Ga）火山岩和片石岩的地球化学：对地球动力环境和大陆增长的影响：讨论

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来源
《GSA Bulletin》 |2007年第4期|487-489|共3页
作者
Guochun Zhao; Alfred Kr?ner;
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作者单位

Department of Earth Sciences, University of Hong Kong, Pokfulam Road, Hong Kong;

Institut für Geowissenschaften, Universit?t Mainz, 55099 Mainz, Germany;

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正文语种 eng
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入库时间 2022-08-17 23:35:14

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1. Geochemistry of Neoarchean (ca. 2.55-2.50 Ga) volcanic and ophiolitic rocks in the Wutaishan greenstone belt, central orogenic belt, North China craton: Implications for geodynamic setting and continental growth: Reply [J] . Ali Polat, Tim Kusky, Jianghai Li GSA Bulletin . 2007,第3a4期

机译：五台山绿岩带，中央造山带，华北克拉通的新新世（约2.55-2.50 Ga）火山岩和脂石岩的地球化学：对地球动力学背景和大陆增长的影响：答复
2. Geochemistry of Neoarchean (ca. 2.55-2.50 Ga) volcanic and ophiolitic rocks in the Wutaishan greenstone belt, central orogenic belt, North China craton: Implications for geodynamic setting and continental growth [J] . Ali Polat, Timothy Kusky, Jianghai Li, GSA Bulletin . 2005,第11a12期

机译：华北克拉通五台山绿岩带，中部造山带的新太古代（约2.55-2.50 Ga）火山岩和蛇绿岩的地球化学：对地球动力学背景和大陆生长的影响
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机译：华北克拉通五台山绿岩带，中央造山带新新世（ca.2.55-2.50 Ga）火山岩和蛇绿岩的地球化学：对地球动力环境和大陆生长的影响：讨论
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Geochemistry of Neoarchean (ca. 2.55-2.50 Ga) volcanic and ophiolitic rocks in the Wutaishan greenstone belt, central orogenic belt, North China craton: Implications for geodynamic setting and continental growth: Discussion

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