Fluid inclusion evidence for petroleum accumulation in northern Qaidam Basin

被引:2
|
作者
Yang Y. [1 ,2 ,3 ]
Li X. [1 ,3 ]
Feng S. [1 ,2 ]
Wang K. [1 ,2 ]
Kong L. [1 ,2 ]
Dong P. [1 ,2 ]
Xu F. [1 ,2 ]
Peng D. [4 ]
Chen Y. [4 ]
机构
[1] State Key Laboratory of Coal Resources and Safe Mining, China University of Mining and Technology
[2] College of Geoscience and Surveying Engineering, China University of Mining and Technology
[3] State Key Laboratory of Petroleum Resource and Prospecting, China University of Petroleum
[4] Research Institute of Exploration and Development, Qinghai Oilfield Company, PetroChina
来源
Chinese Journal of Geochemistry | 2010年 / 29卷 / 04期
基金
中国国家自然科学基金;
关键词
fluid inclusion; grain with oil inclusions (GOI); homogenization temperature; hydrocarbon charging period; oil and gas reservoir; petroleum accumulation;
D O I
10.1007/s11631-010-0475-1
中图分类号
学科分类号
摘要
Based on the results of fluid inclusion study (microscopic characteristics, homogenization temperatures and grains with oil inclusions), the pool-forming time of the Nanbaxian and Mabei 1 oilfields in northern Qaidam Basin was discussed in this paper. Fluid inclusions in northern Qaidam Basin are relatively abundant, including aqueous inclusions and hydrocarbon inclusions. These inclusions are small (5-10 μm), and mainly distributed in quartz fissures, overgrowths and cementations. The abundances of grains with oil inclusions (GOI) are commonly low. The GOI values of most samples are between 2.0%-10.5%, and those of about 40 percent of total samples exceed 5%. The homogenization temperatures of fluid inclusions in different samples are markedly dissimilar, indicating that these inclusions were formed in different periods. According to the measured homogenization temperatures of fluid inclusions and in combination with burial history and thermal evolution history, the Nanbaxian and Mabei 1 oilfields are deduced, which have experienced two hydrocarbon charging periods, with the former of N1-N21 and N22-N23, and the latter of N1 and N1 end -N2, respectively. © 2010 Science Press, Institute of Geochemistry, CAS and Springer Berlin Heidelberg.
引用
收藏
页码:422 / 430
页数:8
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