新疆石油地质 ›› 2006, Vol. 27 ›› Issue (5): 600-603.

• 应用技术 • 上一篇    下一篇

流体包裹体在准噶尔盆地油气成藏研究中的应用

李伟1, 张枝焕1, 杨永才1, 孟凡魏2, 黄宇营3, 秦黎明1   

  1. 1.中国石油大学石油天然气成藏机理教育部重点实验室, 北京 102249;
    2.中国科学院南京古生物研究所, 南京 210008;
    3.中国科学院高能物理研究所同步辐射实验室, 北京 100039
  • 收稿日期:2006-01-23 修回日期:2006-03-22 出版日期:2006-10-01 发布日期:2020-10-20
  • 作者简介:李伟(1979-), 男, 山东郓城人, 在读博士研究生, 石油地质,(Tel) 010-89734164(E-mail) echolw@163.com.
  • 基金资助:
    国家自然科学基金, 高蜡凝析油化学组成剖析和成因机理研究(40172056)资助

Application of Fluid Inclusion to Research of Oil-Gas Accumulations in Junggar Basin

LI Wei1, ZHANG Zhi-huan1, YANG Yong-cai1, MENG Fan-wei2, HUANG Yu-ying3, QIN Li-ming1   

  1. 1. Key Laboratory of Hydrocarbon Accumulation Mechanism, Ministry of Education, China University of Petroleum, Beijing 102249, China;
    2. Nanjing Institute of Geology and Palaeontology, CAS, Nanjing, Jiangsu 210008, China;
    3. Synchrotron Radiation Laboratory, Institute of High Energy Physics, CAS, Beijing 100039, China
  • Received:2006-01-23 Revised:2006-03-22 Online:2006-10-01 Published:2020-10-20

摘要: 应用同步辐射X 射线荧光微探针(SRXRF) 无损分析技术,对准噶尔盆地中部Ⅰ区块两口井侏罗系储集层砂岩中与含油包裹体共生的盐水包裹体进行了微区分析。结果表明,庄1 井和征1 井的包裹体样品同步辐射X 射线能谱图各元素净峰面积存在一定差别,通过标样对K、Ti、Mn、Fe、Ni、Cu、Sr 等元素含量进行了标定,除Fe 含量变化大外,其他元素含量都有较大差别,认为庄1 井和征1 井成藏流体性质差别较大,推测庄1 井与征1 井侏罗系油藏具有不同的成藏史,其油源也是有差别的。这也得到了流体包裹体均一化温度和全岩含油包裹体成分分析的佐证。

关键词: 准噶尔盆地, 盐水包裹体, 微量元素, 均一化温度

Abstract: The saline inclusions in the authigenic minerals of sandstone reservoirs of Jurassic from two wells in Block-1 of center Junggar basin are measured by synchrotron radiation X-ray microprobe techniques. Some element contents, such as K, Ti, Mn, Fe, Ni, Cu and Sr, are calibrated by NIST SRM 612 typical sample. The results show that the microelement contents (except for Fe) of saline inclusions of Well Zhuang-1 and Well Zheng-1 are distinctly different. It is predicted that the reservoirs of Jurassic in Well Zhuang-1 and Well Zheng-1 are different in hydrocarbon accumulation and oil source, for their fluid properties are in big difference. The analysis of the homogenization temperature and the oil-bearing fluid inclusions of whole core confirm the conclusion above.

Key words: Junggar basin, saline inclusion, microelement, homogenization temperature

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