摘要
该文根据塔河油田下奥陶统碳酸盐岩盐水包裹体观察测试资料,对其类型和特征进行了描述,并结合地质分析,重点讨论了盐水包裹体在塔河油田下奥陶统碳酸盐岩成岩作用中的应用。研究表明,除了利用传统的显微镜观察、阴极发光、扫描电镜等分析手段外,利用盐水包裹体所记录的成矿流体信息可以进一步探讨成岩作用,从而为储层预测与研究提供依据。
Based on the observation and test data of the Lower Ordovican carbonate rock salt-water inclusion in Tahe Oilfield, this article gives a description on its type and charateristics. Together with geologic analysis, we discuss the application of salt-water inclusion in the Lower Ordoviaian carbonate rock diagenesis in Tahe Oilfield, and proves the formation and evolution of reservoirs. The research indicates that, despite the traditional analysis ways of microscopic inspection, cathodoluminescence and scanning electron microscope, the mineralizing fluid information from salt-water inclusion can be used to further study ofdiagenesis, and provide basis for reservoir prediction.
出处
《石油实验地质》
CAS
CSCD
2003年第B11期601-606,共6页
Petroleum Geology & Experiment
基金
中国石化新星公司重点科技项目(XYK2001-47-1).
