大洋钻探与西太平洋构造

doi:10.11867/j.issn.1001-8166.1995.03.0234

地球科学进展

1995, Vol. 10

Issue (3): 234-239 DOI: 10.11867/j.issn.1001-8166.1995.03.0234

干旱气候变化与可持续发展

大洋钻探与西太平洋构造

金性春

同济大学海洋地质系上海 200092

OCEAN DRILLING PROGRAM AND TECTONICS OF THE WESTERN PACIFIC REGION

Jin Xingchun

Marine Geology Department,Tongji University,Shanghai 200092

全文: PDF(2526 KB)

摘要：

菲律宾海的深海钻探证实了弧间扩张和残留弧形成模式。小笠原—马里亚纳弧前区的钻探表明，俯冲带初生时伴随着海底扩张，形成了异常宽阔的火山活动带。有许多陆上蛇绿岩形成于俯冲带初生时的海底扩张环境。日本海的钻探揭示了日本边缘盆地的打开和关闭。新近形成的日本海东缘板块边界对华北地区的构造有重要制约作用。中国东海和南海占有独特的构造位置，布置大洋钻探意义重大。文章还强调了中国地质学家从全球地质学的观点研究问题(而不仅仅局限于中国地区)的重要性。

关键词： 边缘盆地; 俯冲带; 菲律宾海; 日本海

Abstract:

The model of the inter-arc spreading and the remnant arc development are verified by the deep-sea drilling in the Philippine Sea. The driling in the Bonin-Mariana forearc shows that the volcanic active zone, which was anomalously large, occurred during the juvenile phase of subduction with sea-floor spreading. Lots of ophiolite found on continent were developed in the setting of sea-floor spreading in the juvenile phase of subduction. The drilling in the Japan Sea reveals processes of opening and closing of the margin basin of Japan Sea.The recent plate boundary at the east margin of Japan Sea imposes important restriction on tectonics in North China. The ocean drilling in the East China Sea and South China Sea will be of great signification because of their distinctive tectonic positions. The present paper emphasizes the significance of approaches to geological problems from global view instead of local one for Chinese geologists.

Key words: Margin basin Subduction zone Philippine Sea Japan Sea.

收稿日期: 1995-02-21 出版日期: 1995-06-01

通讯作者: 金性春

作者简介: 金性春，男，1942年6月出生，副教授，主要从事海洋地质和大地构造学研究.

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引用本文:

金性春. 大洋钻探与西太平洋构造[J]. 地球科学进展, 1995, 10(3): 234-239.

Jin Xingchun. OCEAN DRILLING PROGRAM AND TECTONICS OF THE WESTERN PACIFIC REGION. Advances in Earth Science, 1995, 10(3): 234-239.

链接本文:

http://www.adearth.ac.cn/CN/10.11867/j.issn.1001-8166.1995.03.0234 或 http://www.adearth.ac.cn/CN/Y1995/V10/I3/234

[1] Sutter J F,Snee L W. K/Ar and ⁴⁰Ar/³⁹Ar dating of basaltic rocks from Deep Sea Drilling Project Leg 59. In:Kroenke L et al (eds).Initial Reports DSDP, Vol 59,1980. 729-734.
[2] Kling S A. Radiolarians from the Mariana Trough and Trench region. In: Hussong D M et al (eds). Initial Reports DSDP,Vol 60. 1981. 537-555.
[3] Fryer P,Pearce J A et al Summary of results from Leg 125. In:Fryer P, Pearce J A et al.(eds). Proceedings ODP, Initial Reports,Vol 125.1990.367-380.
[4] Taylor B. Rifting and the volcanic-tectonic evolution of the Izu-Bonin Mariana arc. In:Taylor B et al (eds). Proceedings ODP.Scientific Reports, Vol 126.1992. 627-652.
[5] Stern R J,Bloomer S H. Subduction zone infancy:Examples from the Eocene Izu-Bonin-Mariana and Jurassic California arcs. Geological Society of America Bulletin,1992,104(12):1621-1636.
[6] Pearce J A,Lippard S J and Roberts S. Characteristics and tectonic significance of supra-subduction zone ophiolites. In: Kokelaar B P and Howells M F eds. Marginal Basin Geology. 1984. 77-94.
[7] Maltman A J,Byrne T,Karig D E. Deformation at the toe of an active accretionary prism:Synopsis of results from ODP Leg 131,Nankai,SW Japan. Journal of Structural Geology,1993,15(8):949-963.
[8] Tamaki K,Suyehiro K et al. Tectonic synthesis and implications of Japan Ses ODP drilling. In:Tamaki K,Suyehiro K et al .Proceedings ODP,Scientific Results,Vol 127/128,Pt 2. 1992. 1333-1348.
[9] Shipboard Scientific Party,Site 796. In:Tamaki K,Pisciotto K et al. Proceedings ODP,Initial Reports, Vol 127. 1990. 247-322.
[10] Kuno H. Lateral variation of basaltic magma type across continental margins and island arcs. Bull Volcanol,1966, 29:195-222.
[11] Sengor A M C. The story of Tethys:How many wives did Okeanos have? Episodes,1985,8:3-12.

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