摘要
本文从地层沉积物孔隙度随深度变化的关系模型入手 ,确定了沉积速率的计算公式 ,研究了中国大陆东部边缘渤海湾盆地的沉积过程 ,为认识古代环境与地质演变提供了一种手段 。
Beginning with relation models showing that porosities of strata deposition change with their depths,this paper decides the calculating formula of deposition rate,and studies the deposition process of Pohai Gulf Basin in the eastern edges of China,thus offers efficient means for understanding the ancient environments and geological evolution,discusses the history and contribution of Yellow River's continent[一making.
出处
《黄河水利职业技术学院学报》
2000年第1期10-13,共4页
Journal of Yellow River Conservancy Technical Institute
关键词
地层
脱压
沉积速率
黄河造陆
strata
cast off pressure
deposition rate
Yellow River's continent一making.