中国东部断陷盆地岩盐样品的仪器中子活化分析

    INAA OF ROCK SALT SAMPLES FROM A BLOCK BASIN IN EAST CHINA

    • 摘要: <正> 地质上蒸发岩是天然卤水在蒸发、浓缩过程中通过化学沉淀而形成的,随着浓缩作用的进行,盐度不断增加。而盐水湖和淡水湖的物理、化学过程很不相同,盐水湖沉淀有机物不易分解且很好地保存下来,沉积物中有机质含量主要取决于这种保存过程。根据报道,蒸发岩与油气之间存在着密切关系,含油极富的中东、苏联、北美、欧洲等地的油气都是贮存在蒸发岩之下或分布于蒸发岩近侧。与此情况相似,中国东部许多新生代含油盆地都发育着巨厚的蒸发岩系。对于规模如此巨大的蒸发岩及其与油气的密切关系,目前引起了人们的极大关注。对于我国东部新生代盆地的地质复杂性,很多地质工作者都是从宏观上对沉积相进行

       

      Abstract: 17 elements including Ca, Sc, Cr, Fe, Co, Zn, Br, Rb, Sr, Ba, La, Ce, Eu, Yb, Hf, Th and U have been determined by INAA for 27 rock salt samples from Zhong Yuan oil field (geologically known as " Dong-pu seg" ) in Henan Province. The samples covering a thickness of 100 m are taken from 3000 m depth under earth surface. NaCl contents are more than 97%. The multielement concentration data have provided important information for the study of origins of the brine and the conditions of its formation. The concentrations of Br are ranging from 8.7 to 46.6 ppm, with an average of 23.5 ppm. On this basis, geologists have concluded that Dong-pu seg were formed from the sedimentation of inland salt paste.Further information on the history of geological structure may be obtained by comparing these results with trace element composition for marine facies evaporation.

       

    /

    返回文章
    返回