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。
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.
出处
《海洋地质动态》
2004年第8期16-19,共4页
Marine Geology Letters
