| 麦哲伦海山链漂移史及可能的来源 |
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| 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. |
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| 作者姓名： | 赵俐红 金翔龙 高金耀 李家彪 初凤友 |
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| 作者单位： | 1.国家海洋局 第二海洋研究所 海底科学重点实验室,浙江 杭州 310012;山东科技大学 地质科学与工程学院,山东 青岛 266510 |
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| 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)。 |
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| 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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| 关 键 词： | 麦哲伦海山链 backtracking方法 hot-spotting方法 法属玻利尼西亚热点群 |
| 收稿时间： | 2009/12/10 0:00:00 |
| 修稿时间： | 2010/2/22 0:00:00 |
The research on the drifting history and possible origin of the Magellan seamount trail |
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| ZHAO Li-hong,JIN Xiang-long,GAO Jin-yao,LI Jia-biao and CHU Feng-you.The research on the drifting history and possible origin of the Magellan seamount trail[J].Acta Oceanologica Sinica (in Chinese),2010,32(3):60-66. |
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| Authors: | ZHAO Li-hong JIN Xiang-long GAO Jin-yao LI Jia-biao and CHU Feng-you |
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| Institution: | 1.Key Laboratory of Submarine Geoscience,Second Institute of Oceanography,State Oceanic Administration,Hangzhou 310012, China;College of Geological Science & Engineering, Shandong University of Sciences and Technology,Qingdao 266510, China2.Key Laboratory of Submarine Geoscience,Second Institute of Oceanography,State Oceanic Administration,Hangzhou 310012, China |
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| Abstract: | The Magellan seamount trail includes tens of isolated guyots trending EW.A backtracking method and a hot-spotting method were used to trace the Magellan seamount trail from the movement of a plate and its geometry based on previous studies in this region. The result shows that the Magellan seamount trail is the collective products of intraplate volcanism originating from multiple hot spots and plate tectogenesis. The Magellan seamount trail is derived from the present French Polynesian hot spots trending NNW during the Cretaceous. They are also affected by the activity of two fracture zones, which trend SN and NNW, and thermal activity with the movement of the plate. Finally the present Magellan seamount trail is formed. |
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| Keywords: | Magellan seamount trail backtracking method hot-spotting method French Polynesian hot spot group |
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