石油与天然气地质 ›› 1986, Vol. 7 ›› Issue (4): 412-418.doi: 10.11743/ogg19860412

• 论文 • 上一篇    下一篇

西沙永乐群岛珊瑚礁一瞥

沙庆安   

  1. 中国科学院地质研究所
  • 收稿日期:1986-01-24 出版日期:1986-12-25 发布日期:2012-01-16

A GLIMPSE OF CORAL REEFS OF THE YONGLE ISLANDS,XISHA ARCHIPELAGO

Sha Qingan   

  1. Institute of Geology, Academia Sinica
  • Received:1986-01-24 Online:1986-12-25 Published:2012-01-16

摘要:

永乐群岛(环礁)由七个分隔的礁体组成,环礁中部泻湖水深约40m。各礁坪有着相似的地貌特征,可分出外斜坡、外凸起、外坪地、岛屿(沙、砾或岩石岛)、内坪地、内斜坡等生物、沉积物各异的相带。全富岛外有二道海滩岩,说明沙岛至少已迁移三次。由岩石构成的石屿岛呈背斜构造,显然为沉积背斜。

Abstract:

Yongle Islands(atoll)is situated in the west of Xisha Archipelago of the South China Sea.It consist of seven bigger separated reefs.The central lagoon of theatoll is about 40min depth.These reef-flats appear a similar in geomorphic features,and can be divided into several zones,including outer-slope,outer-crest,outer-flat,island(sand,gravel or rock island),inner-flat,inner-slope.Each zone has its own organisms and sediment features.Two lines of beachrocks occur outside the Quanfu Island.This indicatesthat the sand island has moved three times at least.Shiyu Island,consisting of cemented rock,appears to be an anticline structure.Obviously,it is a deposi-ting anticline.