论文

海南岛潮汐汊道的现代沉积特征研究*

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  • 1. 首都师范大学地理系 北京 100073;
    2. 南京大学大地海洋科学系 南京 210093;
    3. 中国科学院国家计委地理研究所 北京 100101

收稿日期: 1995-10-13

  修回日期: 1996-02-28

  网络出版日期: 1996-06-15

基金资助

* 南京大学海岸与海岛开发国家试点实验室支助

A STUDY ON SURFACE SEDIMENTRY CHARACTERISTIC OF TIDAL INLETS IN HAINAN AN ISLAND

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  • 1. Department of Geography, Capital Normal Uniuersity Beijing 100037;
    2. The department of Geo & Ocean Sciences, Nanjing Uniuersity Nanjing 210093;
    3. Institute of Geography, Chinese Academy of Sciences Beijing 100101

Received date: 1995-10-13

  Revised date: 1996-02-28

  Online published: 1996-06-15

摘要

海南岛存在着大量港湾溺谷型和砂坝泻湖型潮汐汊道。本文以两类潮汐汊道的典型──三亚砂坝泻湖型潮汐汊道和洋浦港湾溺谷型潮汐汊道为例,分析了两类潮汐汊道的成因和地貌发育体系;研究了两类潮汐汊道的现代沉积特征(粒度、重矿、地球化学、有孔虫);对比了两类潮汐汊道的发育模式和沉积模式;探讨了两类潮汐汊道的稳定性。

本文引用格式

邵全琴, 王颖, 赵振家 . 海南岛潮汐汊道的现代沉积特征研究*[J]. 地理研究, 1996 , 15(2) : 84 -91 . DOI: 10.11821/yj1996020011

Abstract

There are many bay-drowned-valley tidal inlets and Sandbar-lagoon tidal inlets in Hainan island.This paper selected two tipical deputies──Yanpu Bay-drowned-valley tidal inlet and Sanya sandbar-lagoon tidal inlet, analysed and compared their geomorphological structure and surface sedimentation.and got some conclutions:(1) The difference and the similarities of developmental models about bay-drowned-valley tidal inlet and sandbar-lagoon tidal inlet:(a) The bay-drowned-valley tidal inlet system has three geomorphological units──tidal inlet and its flood tidal delta, ebb tidal delta.and so does sand bar-lagoon tidal inlet system; (b) The developmental scale of bay-drownedvalley tidal inlet is greater than that of Sanya sandbar-lagoon tidal inlet; (c) The developmental coefficients of flood tidal delta and ebb tidal delta of Yanpu tidal inlet are 0.12 and 0.44 respectively,those of Sanya tidal inlet are 1 and 2.8 respectively.(2) The difference and similarities of sedimentary models about bay-drowned-valley tidal inlet and sandbar-lagoon tidal inlet:(a) In Yanpu baydrowned-valley tidal inlet, the grain size of sediments in tidal inlet is smaller than that on ebb tidal delta and flood tidal delta.In Sanya sandbar-lagoon.the grain size of sediments is greater than that on ebb tidal delta and flood tidal delta; (b) The grain size of sediments on all geomorphological units of bay-drowned-valley tidal inlet system is smaller than that of sandbar-lagoon tidal inlet system;(c) The heavy mineral contents and ZTR of sediments in Yanpu bay-drowned-valley tidal inlet are higher than those in Sanya sand bar-lagoon tidal inlet:(d) The heavy mineral combinations of sediments on bay-drowned-valley inlet and its ebb delta and flood tidal delta are different.The heavy mineral combinations of sediments on sandbar-lagoon tidal inlet and its ebb delta and nab tidal delta are the same; (e) The foraminifer genus-Ammonia and Elphdium are common in both of the two type tidal inlets; (f) The sediments of Sanya Yuzan stream outlet have many Nummulites and Cellanthas, but that in the Yanpu area has no such materials.(3) The stability of bay-drowned-valley tidal inlet in better than that of sand-bar-lagoon tidal inlet.
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