| 地幔柱研究述评 |
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| 引用本文： | 周连成,白伟明,赵俐红,陆凯.地幔柱研究述评[J].海洋地质动态,2004,20(8):16-19. |
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| 作者姓名： | 周连成 白伟明 赵俐红 陆凯 |
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| 作者单位： | 青岛海洋地质研究所,青岛,266071;青岛海洋地质研究所,青岛,266071;中国海洋大学,青岛,266003;国家海洋局第二海洋研究所,杭州,310012 |
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| 摘 要： | 地幔柱与热点既可见于板块内部，也可见于洋中脊和造山带等板块边界，既可见于现代更可见于古代，因而它可能影响到地表各处的成矿作用。简单介绍了地幔柱特征、类型及其在富钴结壳成矿作用中的地位。
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| 关 键 词： | 地幔柱 热点 成矿作用 |
| 文章编号： | 1009-2722(2004)08-0016-04 |
| 修稿时间： | 2004年4月13日 |
Comments on the Studies of Mantle Plumes |
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| ZHOU Lian-cheng.Comments on the Studies of Mantle Plumes[J].Marine Geology Development,2004,20(8):16-19. |
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| Authors: | ZHOU Lian-cheng |
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| Institution: | ZHOU Lian-cheng~ |
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| Abstract: | Mantle plumes and hotspots can be either found in the interior of a plate or along the boundaries of plates such as mid oceanic ridge and orogenic zone, and either in modern or ancient times, and therefore they could have influenced mineralization in the surface layers of the Earth. Characteristics and types of mantle plumes and their roles in the mineralization of Co-rich crusts are briefly introduced. |
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| Keywords: | mantle plume hotspot mineralization |
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