琼州海峡成因与时代

赵焕庭; 王丽荣; 袁家义

琼州海峡成因与时代

1 中国科学院边缘海地质重点实验室, 广州 510301;
2 中国科学院南海海洋研究所, 广州 510301;
3 中山大学地球科学系, 广州 510275

基金项目:

国家自然科学基金项目(40572102)

广东省社会发展攻关项目(2003A3050103)

中国科学院知识创新工程重要方向性项目(kzcx2-yw-318)

国家科技计划课题(2006BAB19B03)

中国科学院边缘海地质重点实验室基金(MSGLO508)

详细信息

作者简介:
赵焕庭(1937-),男,研究员,从事海洋地质研究,E-mail:wlrlwqyshq@yahoo.com.cn

中图分类号: P736.2
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- 文章访问数: 2776
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出版历程
- 收稿日期: 2006-11-09
- 修回日期: 2007-01-07

ORIGIN AND TIME OF QIONGZHOU STRAIT

1 CAS Key Laboratory of Marginal Sea Geology, Guangzhou 510301, China;
2 South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China;
3 Department of Geosciences, Zhongshan University, Guangzhou 510275, China

摘要

摘要: 琼州海峡的成因有海岸侵蚀说、构造断裂说和海侵低地说,海南岛与雷州半岛分离的时代有上新世、第四纪初、中更新世之前、中更新世之后或全新世等几种说法。分析了琼州海峡地质、海洋和区域古生物地理等新资料后认为,琼州海峡不是断裂谷,其前身是常态低地,是在全新世中期全球性海侵淹没峡区原来的常态低地而成的,主要形成时段为(10 570±560)~(7 125±96) aBP;推算自琼州海峡形成以来,中央深槽下切平均速度为0.7 cm/a,西口外潮流三角洲堆积平均速率为0.17~0.31 cm/a。
- 全新世中期海侵 /
- 琼州海峡 /
- 海南岛 /
- 雷州半岛
Abstract: The origin of Qiongzhou Strait has 3 causes:coast erosion, tectonic rifing and marine transgression. And the time for Hainan Island and Leizhou Peninsula to separate from each other also has some explanations:Pliocene, the beginning of Quaternary, before middle Pleistocene, after middle Pleistocene and Holocene. The latest data about the geology, oceanography and regional palaeo-biogeography of Qiongzhou Strait are analyzed in the paper, and it is thought that Qiongzhou Strait is not a rift. It grew out of a normal low land, and was formed in the middle Holocene, about (10 570±560)~(7 125±96) aBP, when marine transgressed the original normal low land. It is inferred that the average speed of central trough valley undercutting is 0.7 cm·a^-1, and the average speed of tidal current delta accumulation outside the west mouth is 0.17~0.31 cm·a^-1 after the Qiongzhou Strait formed.
- middle Holocene transgression /
- Qiongzhou Strait /
- Hainan Island /
- Leizhou Peninsula

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