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[1]段博林,苏 犁*,王 静,等.扬子板块西北缘新元古代洋县桑溪沟花岗岩成因: Rodina 超大陆裂解与地壳重熔[J].地球化学,2018,47(05):506-521.[doi:10.19700/j.0379-1726.2018.05.005]
 DUAN Bo-lin,SU Li*,WANG Jing and XIAO Liang.Origin of Neoproterozoic complexes in the northwestern margin of the Yangtze plate Sangxigou granite: Breakup of the Rodinia supercontinent and melting of the crust[J].Geochimica,2018,47(05):506-521.[doi:10.19700/j.0379-1726.2018.05.005]
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扬子板块西北缘新元古代洋县桑溪沟花岗岩成因: Rodina 超大陆裂解与地壳重熔

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备注/Memo

收稿日期(Received): 2017-05-15; 改回日期(Revised): 2017-11-04; 接受日期(Accepted): 2017-11-20
基金项目: 国家自然科学基金(40572045)
作者简介: 段博林(1992–), 男, 硕士研究生, 矿物学、岩石学、矿床学专业。E-mail: duanbolin@cugb.edu.cn
* 通讯作者(Corresponding author): SU Li, E-mail: suli@cugb.edu.cn; Tel: +86-10-82322858

更新日期/Last Update: 2018-09-30