摘要
研究了南海南部大陆架的残留沉积物的粒度、石英砂表面结构特征、生物分布等，并指出残留沉积普遍遭受改造。按其早期的形成环境差异和改造作用不同，划分出加里曼丹－巴拉望残留沉积区和亚南巴斯－纳土纳残留沉积区。
he grain-size, quartz sand grain surface tectures, biological sedimentation and chemistry of the relict sediments in the south shelf of South China Sea were studied.Generally. the relict sediments had already been transformed. According to different transformation,there are two kinds of relict sediment regions, which are the Kalimantanpalawan and Natuna Is. Anambas Is. region.
出处
《热带海洋》
CSCD
1994年第3期47-53,共7页
关键词
残留沉积
南海
大陆架
elict sediment, shelf, South China Sea
