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南沙群岛永暑礁90多万年以来的海平面变化

THE CHANGE OF SEA-LEVEL OF YONGSHU REEF IN NANSHA ISLANDS SINCE 900 000 YEARS B.P.

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【作者】 赵焕庭孙宗勋宋朝景朱袁智陈欣树沙庆安

【Author】 Zhao Huanting; Sun Zongxun; Song Chaojing; Zhu Yuanzhi;Chen Xinshu; Sha Qingan(South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301)(geological Institute, Chinese Academy of Sciences, Beijing 100029)

【机构】 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

【摘要】 于1990年5-6月在永暑礁礁坪上打一全采芯的地质研究钻井,编号为南永1井,总进尺为15207m,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目早更新世晚期以来经历了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。

【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.

【基金】 中国科学院南沙综合科学考察队调查研究报告!D-00042
  • 【文献出处】 海洋与湖沼 ,Oceanologia Et Limnologia Sinica , 编辑部邮箱 ,1996年03期
  • 【分类号】P731.23
  • 【被引频次】15
  • 【下载频次】222
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