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地球科学进展  2009, Vol. 24 Issue (12): 1331-1338    DOI: 10.11867/j.issn.1001-8166.2009.12.1331
IODP研究     
地球深部与表层的相互作用
汪品先
同济大学海洋地质国家重点实验室,上海200092
Interactions between Earth′s Deep and Surface
WANG Pinxian
State Key Laboratory of Marine Geology, Tongji University, Shanghai200092,China
 全文: PDF(5319 KB)  
摘要:

板块理论和全球变化是20世纪地球科学中的2大突破性进展。进入21世纪,地球系统科学进入将这两方面结合起来,探索地球深部和表层系统的相互作用,即“固体地球动力学与行星循环(planetary cycle)”的新阶段。根据最近国际综合大洋钻探计划关于2013年后学术新方向的讨论,从俯冲带加工厂、大洋中脊与巨型火成岩省3个方面进行介绍,提出我国打破传统的学科界限、迎接新方向的建议。

关键词: 地球系统深部过程表层系统行星循环大洋钻探    
Abstract:

The Plate Tectonics and Global Changes were two major breakthroughs in Earth science over the 20th century. A new focus of Earth science in the 21st century will be the interactions between the Earth′s deep and surface systems, i.e. “solid Earth dynamics and planetary cycle”. The present paper briefly discusses the new research frontiers on the basis of the IODP meeting on its scientific targets beyond 2013, including three parts: Subduction factory, mid-ocean ridge, and large igneous province. The paper ends with a suggestion that China has to develop cross-disciplinary studies to meet the new targets in Earth science.

Key words: Earth system    Deep processes    Surface system    Planetary cycle    Ocean drilling
收稿日期: 2009-12-16 出版日期: 2009-12-17
:  P31  
基金资助:

国家重点基础研究发展计划项目“大洋碳循环与气候演变的热带驱动”(编号:2007CB815900);国家高技术研究发展计划重点项目“大洋钻探站位调查关键技术研究”(编号:2008AA093001)资助.

通讯作者: 汪品先(1936-),男,江苏苏州人,教授,中国科学院院士,主要从事古海洋学及古环境研究.     E-mail: pxwang@online.sh.cn
作者简介: 汪品先(1936-),男,江苏苏州人,教授,中国科学院院士,主要从事古海洋学及古环境研究. E-mail:pxwang@tongji.edu.cn
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汪品先

引用本文:

汪品先. 地球深部与表层的相互作用[J]. 地球科学进展, 2009, 24(12): 1331-1338.

WANG Pinxian. Interactions between Earth′s Deep and Surface. Advances in Earth Science, 2009, 24(12): 1331-1338.

链接本文:

http://www.adearth.ac.cn/CN/10.11867/j.issn.1001-8166.2009.12.1331        http://www.adearth.ac.cn/CN/Y2009/V24/I12/1331

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