摘要
本文论述了松辽盆地北部杨大城子地层水中微量金属元素组成,研究了地层水中微量金属元素含量的分布特征.研究结果表明,杨大城子地层水中各种元素总的含量特征是Fe>Sr>Zn>Mn>Cu>Ni>Cr。Ni/Cu和Mn/Fe的比值,因地区不同具有明显的差异。平面上地层水中金属元素含量与储层的含油气性有关,含油气区地层水中金属元素含量高,接近含油气区次之,远离含油气区最低。
This paper discussed the components and content distribution of trace metal elements in stratigraphic water. The result shows that the content of various metal elements is Fe>Sr>Zn>Mn>Cu>Ni>Cr in stratigraphic water of the Yangdachengzi oil-bearing formation. Ratio of Ni/Cu and Mn/Fe is obviously different in various areas. The content of metal elememts in stratigraphic water is concerned with the hy drocarbon-bearing property of reservoir on the plane. The content of metal elements is gradually decreased from oil and gas bearing areas to water bearing areas.
出处
《石油实验地质》
CAS
CSCD
北大核心
1998年第2期160-165,共6页
Petroleum Geology & Experiment
基金
油气藏地质和开发工程国家重点实验室资助