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马朗凹陷马1井储层长石中有机包裹体研究

张小青, 伊海生, 危国亮, 张小芹

张小青, 伊海生, 危国亮, 张小芹. 马朗凹陷马1井储层长石中有机包裹体研究[J]. 沉积与特提斯地质, 2005, 25(4): 83-86.
引用本文: 张小青, 伊海生, 危国亮, 张小芹. 马朗凹陷马1井储层长石中有机包裹体研究[J]. 沉积与特提斯地质, 2005, 25(4): 83-86.
ZHANG Xiao-qing, YIN Hai-sheng, WEI Guo-liang, ZHANG Xiao-qin. Approaches to the organic inclusions from feldspar in the Ma-1 well reservoirs in the Malang depression[J]. Sedimentary Geology and Tethyan Geology, 2005, 25(4): 83-86.
Citation: ZHANG Xiao-qing, YIN Hai-sheng, WEI Guo-liang, ZHANG Xiao-qin. Approaches to the organic inclusions from feldspar in the Ma-1 well reservoirs in the Malang depression[J]. Sedimentary Geology and Tethyan Geology, 2005, 25(4): 83-86.

马朗凹陷马1井储层长石中有机包裹体研究

详细信息
    作者简介:

    张小青,1969年生,博士生,从事含油气盆地分析及油气储层研究。

  • 中图分类号: P575.4

Approaches to the organic inclusions from feldspar in the Ma-1 well reservoirs in the Malang depression

  • 摘要: 根据对马朗凹陷马1井储层长石中有机包裹体的基本特征、均一温度、荧光及荧光光谱分析,得出有机包裹体均一温度为60 ~ 90℃及120~ 140℃,其对应的荧光颜色分别为黄色和蓝绿色。认为储层的油气运移经历了两期,第一期为烃类的主要运移、聚集期,油气为低成熟油;第二期为少量的烃类聚集,并判断出二叠系条湖组该段储层为油气产层。
    Abstract: The integration of general characteristics,homogenization temperatures, fluorescence and fluorescence spectrum of the organic inclusions from feldspar in the Ma-1 well reservoirs in the Malang depression indicates that the organic inclusions have the homogenization temperatures ranging between 60-90℃ and 120-140℃,correspondingly with the yellow fluorescence and blueish green fluorescence,respectively.The oil and gas from the reservoirs have gone through two phases of migration: Phase 1,hydrocarbon migration and accumulation as low-maturity oil,and Phase 2,the accumulation of hydrocarbons.These reservoirs in the Permian Tiaohu Formation are believed to be productive.
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出版历程
  • 收稿日期:  2005-02-27
  • 发布日期:  2005-12-29

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