| Nd Isotopic Characteristics of Granitoids from the New foundland Appalachians |
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| 作者姓名： | WANG Chaoyang WANG Tao Cees Van STAAL LIN Shouf ZHANG Jianjun |
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| 摘 要： | 正The Appalachian orogen in North America is currently considered to be a Paleozoic accretion-type orogenic belt,or a collage,formed by collision of many ancient blocks between Laurentian and Gondwanan margins (Williams,1979;Williams et al.,1988;van Staal et al.,2007).Recently,major progress has been made in understanding the characteristics and tectonic evolution of the outboard peri-Laurentian and peri-Gondwanan terranes of the Iapetus Ocean (van Staal et al.,2009,2012).
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Nd Isotopic Characteristics of Granitoids from the New foundland Appalachians |
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| Authors: | WANG Chaoyang WANG Tao Cees Van STAAL LIN Shoufa and ZHANG Jianjun |
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| Institution: | 1 Key Laboratory of Deep-Earth Dynamics, Ministry of Natural Resources, Institute of Geology, China
Academy of Geological Sciences, Beijing 100037, China,1 Key Laboratory of Deep-Earth Dynamics, Ministry of Natural Resources, Institute of Geology, China
Academy of Geological Sciences, Beijing 100037, China;2 Beijing SHRIMP Center, Beijing, 100037, China,3 Geological Survey of Canada, 1500-605 Robson Street, Vancouver, BC V6B 5J3, Canada,4 Department of Earth and Environmental Sciences, University of Waterloo, Waterloo, Ontario, Canada and 1 Key Laboratory of Deep-Earth Dynamics, Ministry of Natural Resources, Institute of Geology, China
Academy of Geological Sciences, Beijing 100037, China |
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