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现代地质 ›› 2013, Vol. 27 ›› Issue (5): 1193-1201.

• 油气成藏机理 • 上一篇    下一篇

利用石油包裹体烃组分信息恢复塔中地区油气成藏过程

姜振学1,2,李峰1,2,李卓1,2   

  1. 中国石油大学(北京)油气资源与探测国家重点实验室,北京 102249
  • 收稿日期:2013-06-20 修回日期:2013-08-03 出版日期:2013-10-17 发布日期:2013-10-31
  • 作者简介:姜振学,男,教授,博士生导师,1963年出生,石油地质学专业,主要从事油气成藏机理研究。 Email: jiang@cup.edu.cn
  • 基金资助:

    国家自然科学基金项目(40972088);国家“973”项目(2011CB201105); 国家油气重大专项项目(2011ZX05003 - 001)

Applying Molecular Compositions of Inclusion Data to Restore Hydrocarbon Charge History in the Tazhong Area

JIANG Zhen-xue1,2,LI Fend1,2, LI Zhuo1,2   

  1. State Key Laboratory of Petroleum Resources and Prospecting ,China University of Petroleum,Beijing 102249
  • Received:2013-06-20 Revised:2013-08-03 Online:2013-10-17 Published:2013-10-31

摘要:

为恢复塔中地区油气成藏过程,利用改进的石油包裹体烃组分分析方法进行了详细的研究。结果表明塔中地区储层油和包裹体油的组分差异明显。包裹体油和下奥陶统储层油中伽马蜡烷和C28甾烷相对丰度较高,来源于寒武系—下奥陶统烃源岩,其他储层油中伽马蜡烷和C28甾烷相对丰度较低,来源于中—上奥陶统烃源岩。储层油的成熟度高于对应层位的包裹体油,表明高成熟度的石油再次充注。石炭系和志留系包裹体油和储层油中存在25-降藿烷系列,表明石油成藏后遭受了生物降解作用。恢复了塔中地区3期油气成藏过程,第1期和第Z期分别为志留纪末期和二叠纪末期来源于寒武系-下奥陶统烃源岩的油气成藏,第3期为二叠纪末期来源于中-上奥陶统烃源岩的油气成藏。

关键词: 塔中地区, 包裹体烃组分, 油气来源, 生物降解作用, 油气成藏过程

Abstract:

In order to restore the hydrocarbon charge history in the Tazhong area,an improved molecular composition of inclusion(MCI ) method is applied using oils from oil-hearing inclusions(FI-oils)and crude oils. The results show that the FI-oils and the crude oils in the Tazhong oil field originated from different source rock intervals and the crude oils are more mature than the FI-oils.  The FI-oils adsorbed and inclusion oils of the reservoir rocks generally have high concentrations of gammacerane and C28 steranes,similar to the Cambrian-Lower Ordovician source rocks. In contrast,the crude oils generally have low concentrations of gammacerane and C28 Steranes,similar to the Middle-Upper Ordovician source rocks.  The coexistence of 25-norhopane and the intact n-alkanes in all crude oils,and the higher concentration of 25-norhopanes in crude oils than in FI-oils,suggest that later non-biodegraded oil continue to charge and mix in the productive intervals during and/or after early biodegradation. Three episodes of oil charge from two source rock intervals can be restored in the Tazhong area.  The first and the second episodes of oil charge,origin of the Cambrian-Lower Ordovician source rocks,were determined in Late Silurian and Late Permian,followed by the third episode of oil charge derived from the Middle-Upper Ordovician source rocks in the Late Permian.

Key words: the Tazhong area, molecular composition of inclusion, hydrocarbon source, biodegradation, hydrocarbon accumulation process

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