华北基性岩墙群的古地磁极及其哥伦比亚超大陆重建意义

侯贵廷, Henry HALLS, Don DAVIS, 黄宝玲, 杨默函, 王传成. 华北基性岩墙群的古地磁极及其哥伦比亚超大陆重建意义[J]. 岩石学报, 2009, 25(3): 650-658.
引用本文: 侯贵廷, Henry HALLS, Don DAVIS, 黄宝玲, 杨默函, 王传成. 华北基性岩墙群的古地磁极及其哥伦比亚超大陆重建意义[J]. 岩石学报, 2009, 25(3): 650-658.
HOU GuiTing, Henry HALLS, Don DAVIS, HUANG BaoLing, YANG MoHan, WANG ChuanCheng. Paleomagnetic poles of mafic dyke swarms from the North China craton and their relevance to the reconstruction of the supercontinent Columbia[J]. Acta Petrologica Sinica, 2009, 25(3): 650-658.
Citation: HOU GuiTing, Henry HALLS, Don DAVIS, HUANG BaoLing, YANG MoHan, WANG ChuanCheng. Paleomagnetic poles of mafic dyke swarms from the North China craton and their relevance to the reconstruction of the supercontinent Columbia[J]. Acta Petrologica Sinica, 2009, 25(3): 650-658.

华北基性岩墙群的古地磁极及其哥伦比亚超大陆重建意义

  • 基金项目:

    国家自然科学基金项目 (40172066, 40314141, 40772121) 和国家973项目 (2009CB219302)

Paleomagnetic poles of mafic dyke swarms from the North China craton and their relevance to the reconstruction of the supercontinent Columbia

  • 从华北克拉通的中西部和东部发育的基性岩墙群获得三个精确定年的实际古地磁极位置(VGPs)。华北克拉通中西部恒山GU岩墙的斜锆石U-Pb年龄为1769±3Ma,该岩墙的古地磁给出古地磁极位置在北纬36°,东经247° (dp=2, dm=4); 华北克拉通东部DY岩墙的斜锆石U-Pb年龄为1620.8±6.9Ma, 获得的古地磁极位置为北纬6.9°东经81.9°(dp=4.31, dm=6.09); 东部另一条岩墙LW4的SHRIMP U-Pb 年龄为1157±18Ma, 获得的古地磁极位置为北纬27.1°东经162°(dp=15.8, dm=18.7)。通过将这三个从基性岩墙获得的华北克拉通古地磁极位置与加拿大地盾的中元古代视极移曲线对比,在中元古代早期(1800~1600Ma),华北克拉通与加拿大地盾一起同属哥伦比亚超大陆,而在中元古代晚期(1600~1200Ma),华北克拉通与加拿大地盾分离,响应哥伦比亚超大陆的最终裂解事件。
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出版历程
收稿日期:  2008-11-26
修回日期:  2009-01-12
刊出日期:  2009-03-31

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