| 大洋钻探与南海的形成 |
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| 引用本文： | 张训华,朱银奎.大洋钻探与南海的形成[J].海洋科学,1996,20(3):42-46. |
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| 作者姓名： | 张训华 朱银奎 |
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| 作者单位： | 地质矿产部海洋地质研究所!青岛266071 |
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| 摘 要： | 南海是太平洋西部边缘海之一。由于其特殊的大地构造位置和复杂的地 质结构，多年来其形成演化一直是地学界研究和争论的焦点。在南海开展大洋钻 探，不仅可以回答南海形成演化方面的一系列问题，而且对于研究边缘海的形成演 化过程和欧亚板块、印一澳板块、太平洋板块的相互作用与影响，以及全球构造运 动都有重要意义。
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| 关 键 词： | 大洋钻探 单向拉张 形成演化 南海海盆 |
| 收稿时间： | 1996/3/10 0:00:00 |
ODP AND THE FORMATION OF THE SOUTH CHINA SEA |
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| Zhang Xunhua and Zhu Yinkui.ODP AND THE FORMATION OF THE SOUTH CHINA SEA[J].Marine Sciences,1996,20(3):42-46. |
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| Authors: | Zhang Xunhua and Zhu Yinkui |
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| Abstract: | The South China Sea is one of the marginal seas in the western Pacific Ocean. As its special tectonic location and complex geological structure, the formation and evolution of the South China Sea become the focus studied and debated by scientists in geology for many years. The results of ODP in the South China Sea may give explanations to the problems about its formation and evolution, and may be helpful and have great significant for the study of the formation and evolution of marginal seas,and for the study of the interaction among Asian Plate, Pacific Plate and Indo-Autralia Plate, and for the study of global interaction. |
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| Keywords: | ODP Unilateral extension Formation and evolution SCS (The South China Sea) |
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