| 大洋钻探与深海热液作用 |
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| 引用本文： | 吴世迎. 大洋钻探与深海热液作用[J]. 地球科学进展, 1995, 10(3): 223-228. DOI: 10.11867/j.issn.1001-8166.1995.03.0223 |
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| 作者姓名： | 吴世迎 |
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| 作者单位： | 国家海洋局第一海洋研究所 |
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| 摘 要： | 在ＤＳＤＰ／ＯＤＰ的２６年钻探中，有近２０个航次钻遇到的热液作用踪迹或热液产物。强调了深海热液作用作为研究海底扩张，地幔物质上涌，新生洋壳生成及火山活动所构成的地壳演化过程，已经成了大洋钻探计划的核心内容之一，并由此在若干重大理论问题上，获得了突破性的发展。
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| 关 键 词： | 大洋钻探 热液作用 海水循环 矿化 成矿 |
OCEAN DRILLING AND DEEP-SEA HYDROTHERMAL ACTIVITY |
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| Wu Shiying. OCEAN DRILLING AND DEEP-SEA HYDROTHERMAL ACTIVITY[J]. Advances in Earth Sciences, 1995, 10(3): 223-228. DOI: 10.11867/j.issn.1001-8166.1995.03.0223 |
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| Authors: | Wu Shiying |
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| Affiliation: | First Institute of Oceanography,SOA,Qingdao 266003 |
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| Abstract: | Deep-sea hydrothermal activities and hydrothermal products which were found dur-ing nearly 20 cruises in the past 26 years of DSDP/ODP are introduced. It is emphasisedthat deep-sea hydrothermal activity, as the study of sea-floor spreading , mantle materialupwelling, new ocean-floor formation and volcanic activities, has been one of the core as-pects in the Ocean Drilling Project. With the study of deep-sea hydrothermal activity,abreak through progress has been obtained in many important theoretical problems. |
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| Keywords: | Ocean Drilling Hydrothermal activity Sea-water circulation Mineral-ization sources. |
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