天然气地质学

流体包裹体在川西南部上三叠统天然气成藏研究中的应用

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  • 1.中国石油天然气集团公司科技部,北京 100007;2.中国石油天然气成藏与开发重点实验室,
    中国石油勘探开发研究院廊坊分院天然气地质所,河北 廊坊 065007;
    3.中油测井技术服务有限责任公司,北京 100101

收稿日期: 2008-11-10

  修回日期: 2009-02-16

  网络出版日期: 2009-04-10

基金资助

国家“973”计划项目(编号:2007CB209503)资助.

Application of Fluid Inclusions to Research on Natural Gas Accumulation in the Upper Triassic of the Southern Part of West Sichuan

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  • 1. The Science and Technology Management Department, PetroChina, Beijing 100007, China; 
    2. Key Laboratory for Natural Gas Accumulation and Development, PetroChina, Langfang Branch of Research
    Institute of Petroleum Exploration and Development, PetroChina, Langfang 065007, China; 
    3. China National Logging Corporation, Beijing 100081, China

Received date: 2008-11-10

  Revised date: 2009-02-16

  Online published: 2009-04-10

摘要

有机流体包裹体是含油气系统中水—岩相互作用的产物,记录了盆地流体生成、运移和演化的信息。系统观测了川西南部邛西、平落坝及白马庙气田上三叠统须二段原生气藏和侏罗系次生气藏储集层的有机包裹体,并选择性地对某些包裹体进行了激光拉曼光谱分析,而后结合构造埋藏史和烃源岩成熟热演化史对川西南部须二段气藏的成藏过程进行了系统分析,认为川西南部须二段气藏的形成过程大致是连续的,经历了印支晚期少量注入,到燕山期大量注入,再到喜马拉雅期调整、少量注入的过程,其主要充注时期为燕山期(195~95 Ma)。该研究成果对认识研究区气藏地质特征、成藏规律和勘探部署有重要的借鉴意义。

本文引用格式

李峰 张莉 李树晶 崔可平 . 流体包裹体在川西南部上三叠统天然气成藏研究中的应用[J]. 天然气地球科学, 2009 , 20(2) : 174 -181 . DOI: 10.11764/j.issn.1672-1926.2009.02.174

Abstract

Fluid inclusions are resulted from the interaction between water and rocks in petroleum systems, and they record the information of the fluid generation, migration and evolution of a basin. The authors carried out an investigation on the type, distribution characteristics, homogenization temperature, salinity and composition of fluid inclusions in late Triassic clastic rocks in the Pingluoba, Qiongxi and Baimamiao gas fields in the southern part of the west Sichuan foreland basin. Some samples were analyzed using laser Raman spectroscopy. And in combination with the buried history and the maturity history of the source rock, the hydrocarbon accumulation process of the second member gas reservoir of Xujiahe Formation in the basin. The second member gas reservoir experienced a continuous process of formation: small charge in the Indonesian period, large charge in the Yanshan period, and adjustment and small charge again in the Himalayan period. The main charge time is 195~95 Ma. The research is very important to reorganize the gas reservoir geology characteristics, hydrocarbon accumulation rules and to make exploration strategies.

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