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天然气地球科学

• 天然气地质学 • 上一篇    下一篇

准噶尔盆地中拐地区佳木河组流体包裹体特征及成藏期次划分

李振华，邱隆伟，孙宝强，唐 勇，玉华，朱士波   

  1. 1.中国石油大学(华东)地球科学与技术，山东 青岛 266580；
    2.黑龙江省大庆市地震局，黑龙江 大庆 163002;
    3.新疆油田公司勘探开发研究院，新疆 克拉玛依 834000
  • 收稿日期:2013-03-21 修回日期:2013-04-18 出版日期:2013-10-10 发布日期:2013-10-10
  • 通讯作者: 李振华xiaojie901@126.com. E-mail:xiaojie901@126.com.
  • 作者简介:李振华(1985-)，男，山东广饶人，博士研究生，主要从事油气地质和油藏描述方面研究. E-mail:xiaojie901@126.com.
  • 基金资助:

    国家科技重大专项(编号:2009ZX05009-002)资助.

Characteristics of Fluid Inclusion and Charging Events of NaturalGas in Permian Jiamuhe Formation of Zhongguai Area,Junggar Basin

LI Zhen-hua, QIU Long-wei, SUN Bao-qiang, TANG Yong, KONG Yu-hua, ZHU Shi-bo   

  1. 1.Earth Science and Technology Institute in China University of Petroleum,Qingdao 266580, China；
    2.Seismological Bureau of Daqing, Daqing 163002, China；
    3.Exploration and Development Research Institute of Xinjiang Oilfield Company, Kelamayi 834000, China
  • Received:2013-03-21 Revised:2013-04-18 Online:2013-10-10 Published:2013-10-10

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摘要：

为确定中拐地区二叠系佳木河组油气藏的充注时间和成藏期次,利用Linkam THMS 600型冷热台和LabRam-010型激光拉曼光谱仪,采用流体包裹体和拉曼测试技术,对储层沸石和方解石中流体包裹体样品进行测试分析。拉曼测试结果显示，佳木河组中主要存在盐水包裹体、CO2包裹体、低饱和烃包裹体和富含CH4包裹体4种包裹体类型；均一温度和冰点均具有明显的双峰特点，均一温度第1峰值为60~80℃，第2峰值为110~120℃；公式法计算的包裹体盐度主要分布在0.73%~3.86%和5.76%~9.2% 2个区间，说明至少存在2期流体活动。在包裹体测试资料基础上，结合埋藏史、构造演化史和烃源岩演化史最终确定佳木河组主要的成藏期次有2期:三叠纪末—早侏罗世(228~206Ma)；早白垩世(145~112Ma)。 

关键词: 中拐地区, 流体包裹体, 拉曼测试, 均一温度, 成藏期次

Abstract:

For the purpose of ascertaining the time of gas charging and the formation period of gas reservoirs of Permian Jiamuhe Formation in Zhongguai area of Junggar Basin,fluid inclusion samples from this field were tested and analyzed using the more advanced testing apparatus and techniques.The results show that the fluid inclusions of this area mainly include brine inclusion、hydrocarbon-bearing CO2 inclusion,lowly saturated hydrocarbon-rich liquid hydrocarbon inclusion and CH4-rich gaseous hydrocarbon inclusion.The homogenization temperature and salinity of the fluid conclusion both have two special peaks,and the peaks of homogenization temperature are 60-80℃ and 100-120℃.Use formula of calculation method inclusions salinity is mainly distributed in 0.73%-3.86% and 5.76%-9.2%,which shows at least 2 times of fluid activities.The main accumulation period of Jiamuhe Formation has 2 periods on the base of inclusion test data and the burial history,tectonic evolution history and thermal evolution of source rocks: from the Late Triassic to Early Jurassic (228-206Ma) and Early Cretaceous (145-112Ma).

Key words: Zhongguai area, Fluid inclusions, Raman test, Homogenization temperature, Accumulation periods

中图分类号: 

  • TE122.1

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