地球科学进展 ›› 1995, Vol. 10 ›› Issue (3): 223 -228. doi: 10.11867/j.issn.1001-8166.1995.03.0223

干旱气候变化与可持续发展 上一篇    下一篇

大洋钻探与深海热液作用
吴世迎   
  1. 国家海洋局第一海洋研究所  青岛  266003
  • 收稿日期:1995-02-21 出版日期:1995-06-01
  • 通讯作者: 吴世迎

OCEAN DRILLING AND DEEP-SEA HYDROTHERMAL ACTIVITY

Wu Shiying   

  1. First Institute of Oceanography,SOA,Qingdao  266003
  • Received:1995-02-21 Online:1995-06-01 Published:1995-06-01

在DSDP/ODP的26年钻探中,有近20个航次钻遇到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。

Deep-sea hydrothermal activities and hydrothermal products which were found during nearly 20 cruises in the past 26 years of DSDP/ODP are introduced. It is emphasized that deep-sea hydrothermal activity, as the study of sea-floor spreading, mantle material upwelling, new ocean-floor formation and volcanic activities, has been one of the core aspects in the Ocean Drilling Project. With the study of deep-sea hydrothermal activity, a break through progress has been obtained in many important theoretical problems.

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