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南沙群岛永暑礁90多万年以来的海平面变化
引用本文:赵焕庭,孙宗勋,宋朝景,朱袁智,陈欣树,沙庆安. 南沙群岛永暑礁90多万年以来的海平面变化[J]. 海洋与湖沼, 1996, 27(3): 264-270
作者姓名:赵焕庭  孙宗勋  宋朝景  朱袁智  陈欣树  沙庆安
作者单位:中国科学院南海海洋研究所!广州,510301,中国科学院南海海洋研究所!广州,510301,中国科学院南海海洋研究所!广州,510301,中国科学院南海海洋研究所!广州,510301,中国科学院南海海洋研究所!广州,510301,中国科学院地质研究所!北京,100029
基金项目:中国科学院南沙综合科学考察队调查研究报告!D-00042
摘    要:于1990年5-6月在永暑礁坪上打一全采芯的地质研究钻井,编号为南永1总进尺为152.07m,对岩芯详细的地质年代学,地层学,相学和岩石学等进行多学科的分析研究,结果表明,永暑礁地区的海平面自早更新世晚期以及经历了4次上升和间隔的3次下降,形成了4个沉积旋回及其间的3个沉积间断。海平面呈波动式上升趋势。

关 键 词:南沙群岛 永暑礁 海平面变化 古气候
收稿时间:1993-02-08
修稿时间:1995-06-19

THE CHANGE OF SEA-LEVEL OF YONGSHU REEF IN NANSHA ISLANDS SINCE 900000 YEARS B.P.
Zhao Huanting,Sun Zongxun,Song Chaojing,Zhu Yuanzhi,Chen Xinshu and Sha Qingan. THE CHANGE OF SEA-LEVEL OF YONGSHU REEF IN NANSHA ISLANDS SINCE 900000 YEARS B.P.[J]. Oceanologia Et Limnologia Sinica, 1996, 27(3): 264-270
Authors:Zhao Huanting  Sun Zongxun  Song Chaojing  Zhu Yuanzhi  Chen Xinshu  Sha Qingan
Affiliation:South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301;South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301;South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301;South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301;South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301;Geological Institute, Chinese Academy of Sciences, Beijing 100029
Abstract:During May and June, 1990, a geological research core at Yongshu Reefflat named core Nanyong-1 (152.07m deep) was drilled. According to the detailedand multidisciplinary data of geochronology, stratigraphy, facies and petrology ofcore Nanyong- 1, the changillg curve of sea-level of Yongshu areas since 900000years B.P. was drewed. Analytical result showed that the sealevel had 4 rises and 3falls intermediately since late stage of Early Pleistocene, and formed 4 sedimentarycycles and 3 sedimentary interruPted surfaees. Generally, the sea-level rose fluctuatedly.
Keywords:Nansha Islands Yongshu Reef Change of sea-level Palaeoclimate Neotectonic movement  
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