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麦哲伦海山链漂移史及可能的来源

赵俐红 金翔龙 高金耀 李家彪 初凤友

赵俐红, 金翔龙, 高金耀, 李家彪, 初凤友. 麦哲伦海山链漂移史及可能的来源[J]. 海洋学报, 2010, 32(3): 60-66.
引用本文: 赵俐红, 金翔龙, 高金耀, 李家彪, 初凤友. 麦哲伦海山链漂移史及可能的来源[J]. 海洋学报, 2010, 32(3): 60-66.
ZHAO Li-hong, JIN Xiang-long, GAO Jin-yao, LI Jia-biao, CHU Feng-you. The research on the drifting history and possible origin of the Magellan seamount trail[J]. Haiyang Xuebao, 2010, 32(3): 60-66.
Citation: ZHAO Li-hong, JIN Xiang-long, GAO Jin-yao, LI Jia-biao, CHU Feng-you. The research on the drifting history and possible origin of the Magellan seamount trail[J]. Haiyang Xuebao, 2010, 32(3): 60-66.

麦哲伦海山链漂移史及可能的来源

基金项目: 山东省教育厅科技计划项目(J08LB53);浙江省博士后科研项目择优资助资金项目;国家海洋局第二海洋研究所基本科研业务费项目(JB0701)。

The research on the drifting history and possible origin of the Magellan seamount trail

  • 摘要: 麦哲伦海山链主要由十多座相对独立的平顶海山组成,呈北西向展布于太平洋海山密集区。结合前人对麦哲伦海山链形成和漂移的认识,从板块运动和几何学角度出发采用backtracking和hot-spotting海山追踪方法对该区海山的起源与形成进行了研究,结果表明,麦哲伦海山链是多热点成因的板内火山和板块构造运动共同作用的产物,最初于白垩纪期间由法属玻利尼西亚热点群西侧呈北北西向排列的热点活动产生,继而受到板块运动与区内近南北向和北北东向两组断裂及其热活化等的改造作用,最后形成了现今看到的平顶海山。
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出版历程
  • 收稿日期:  2009-12-10
  • 修回日期:  2010-02-22

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