吉林大学学报(地球科学版) ›› 2017, Vol. 47 ›› Issue (2): 355-369.doi: 10.13278/j.cnki.jjuese.201702103

• 地质与资源 • 上一篇    下一篇

白云岩化作用类型及机理——以歧口凹陷古近系沙河街组一段为例

高福红1, 张永胜1, 蒲秀刚2, 杨杨3, 张鐘月4   

  1. 1. 吉林大学地球科学学院, 长春 130061;
    2. 大港油田勘探开发研究院, 天津 300280;
    3. 长春工程学院勘查与测绘工程学院, 长春 130021;
    4. 辽宁省地震局, 沈阳 110034
  • 收稿日期:2016-06-25 出版日期:2017-03-26 发布日期:2017-03-26
  • 作者简介:高福红(1963),女,教授,博士生导师,主要从事岩石学方面的研究,E-mail:gaofh@jlu.edu.cn
  • 基金资助:
    国家自然科学基金项目（41502145）；吉林省教育厅"十三五"科学技术研究规划项目（2016-0313）

Type of Dolomization and Formation Mechanism: A Case Study of Palaeogene Es1 in Qikou Sag

Gao Fuhong1, Zhang Yongsheng1, Pu Xiugang2, Yang Yang3, Zhang Zhongyue4   

  1. 1. College of Earth Sciences, Jilin University, Changchun 130061, China;
    2. Research Institute of Exploration and Development, Dagang Oilfield Company, PetroChina, Tianjin 300280, China;
    3. School of Prospecting & Surveying Engineering, Changchun Institute of Technology, Changchun 130021, China;
    4. Earthquake Administration of Liaoning Province, Shenyang 110034, China
  • Received:2016-06-25 Online:2017-03-26 Published:2017-03-26
  • Supported by:
    Supported by the National Natural Science Foundation of China(41502145)and Science and Technology Research Program of the 13th Five-Year from Education Department of Jilin Province(2016-0313)

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摘要： 通过镜下鉴定和地球化学分析对歧口凹陷古近系沙一段白云岩进行了研究，综合分析了研究区发育的岩石类型及其成因。结果表明：研究区发育泥-微晶白云岩、灰质白云岩、白云质灰岩及少量颗粒白云岩；Sr/Ba值为0.4~4.9，V/Ni值为1.3~7.1，Z值（盐度指数）分布在122.6~162.5；87Sr/86Sr值和同期海水极为接近，因此推断湖盆遭受了海侵作用，海侵为白云岩化作用提供了Mg2+；有序度分布在0.22~0.53，整体较低；Mg/Ca值为0.73~0.91，反映了富钙低镁的特征，表明白云岩形成于准同生阶段。碳氧同位素分析表明，研究区白云岩形成于浅埋藏环境，并且受到了发酵作用的影响，异常高的Sr值也反映了微生物活动的存在。通过以上证据推断本区白云岩是在准同生期、浅埋藏环境、经渗透回流作用形成的，并且受到了发酵作用的影响。

关键词: 古近系, 白云岩化, 碳氧同位素, 歧口凹陷

Abstract: In terms of the microscopic identification and geochemical analysis, study has been made on the dolostones of Palaeogene Es1 in Qikou sag. The result shows that there are microcrystalline-micritic dolomite, calcite dolomite, dolomite limestone, and a little grain dolomite. Sr/Ba ratio is from 0.4 to 4.9, V/Ni ratio is from 1.3 to 7.1, Z value distributed between 122.6~162.5, 87Sr/86Sr ratio of dolostone is extremely close to the seawater. According to the mentioned values, the lake basin was influenced by transgression activity, which brought a large number of Mg2+ for dolomization. The order degree of dolomite is between 0.22-0.53, Mg/Ca ratio is between 0.73-0.91, it has characteristics of rich in Ca2+ and poor in Mg2+, which indicates that the dolostone was formed during the penecontemporaneous period. Carbon and oxygen isotope analysis implies that the dolostone was formed in shallow burial environment, the extremely positive δ13C anomaly indicates that the process of dolomization was affected by fermentation, the abnormal high Sr value suggests an activity of bacteria. Based on the analysis above, the dolostone was formed in shallow burial environment during the penecontemporaneous period by the process of seepage-reflux and the process was affected by methanation.

Key words: Palaeogene, dolomization, carbon and oxygen isotopes, Qikou sag

中图分类号: 

  • P581
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