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南海北部莺歌海—琼东南盆地晚第三纪层序地层与海平面变化
引用本文:郝诒纯,陈平富,万晓樵,董军社.南海北部莺歌海—琼东南盆地晚第三纪层序地层与海平面变化[J].现代地质,2000,14(3):237-245.
作者姓名:郝诒纯  陈平富  万晓樵  董军社
作者单位:1. 中国地质大学地球科学与资源学院,北京,100083
2. 中国科学院古脊椎动物与古人类研究所,北京,100044
摘    要:莺歌海—琼东南盆地自晚第三纪海侵以来 ,可划分出 3个二级层序和 1 3个三级层序 ,利用生物化石 (主要为浮游有孔虫 )基准面确定层序的界面年龄值 ,自上而下分别为 1 .9Ma、2 .2Ma、 2 .8Ma、 3 .4 Ma、 5.1 Ma、 6.0 Ma、 1 0 .2 Ma、 1 2 .6Ma、 1 5.2 Ma、 1 9.6Ma、 2 1 .0 Ma、2 3 .7Ma、 2 5.5Ma、 3 0 Ma。通过各层序沉积期的环境演变 ,探讨了海平面变化的周期性 ,并与同时代的全球海平面旋回作了对比。本区最高海平面时期为早上新世 ,即相当于浮游有孔虫N1 9带至 N2 1 带下部 ,其次为中中新世早期 ,相当于浮游有孔虫 N9至 N1 2 带。

关 键 词:莺歌海—琼东南盆地  第三纪  层序地层学  海平面变化  沉积环境
修稿时间:2000-05-08

Late Tertiary sequence stratigraphy and sea level changes in Yinggehai-Qiongdongnan basin
HAO Yichun ,CHEN Ping fu,WAN Xiao qiao ,DONG Jun she.Late Tertiary sequence stratigraphy and sea level changes in Yinggehai-Qiongdongnan basin[J].Geoscience——Journal of Graduate School,China University of Geosciences,2000,14(3):237-245.
Authors:HAO Yichun  CHEN Ping fu  WAN Xiao qiao  DONG Jun she
Institution:HAO Yichun 1,CHEN Ping fu2,WAN Xiao qiao 1,DONG Jun she 2
Abstract:Thirteen depositional sequences are presented based on the analyses of well logs and seismic data in Late Tertiary in Yinggehai Qiongdongnan basin, the northern part of South China Sea.The ages of 13 depositional sequence boundaries are dated by bio datum planes (planktonic foraminifera)as 1 9, 2 2, 2 8, 3 4, 5 1, 6 0, 10 2, 12 6, 15 2, 19 6, 21 0, 23 7, 25 5 and 30 0 Ma respectively.The cycles of relative sea level changes are discussed systematically according to the depositional systems and sedimentary facies.The highest stand of sea level developed in Middle and Lower Pliocene,approximately in the interval between the N 19 and the lower part of N 21 planktonic foraminiferal zones. Another high stand of sea level happened in Middle Miocene, roughly from the N 9 to the N 12 planktonic foraminiferal zones.The cycles of relative sea level changes can be correlated with that of Haq et al.(1987).
Keywords:Yinggehai Qiongdongnan basin  Tertiary  sequence stratigraphy  sea level change  depositional system
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