High molecular weight (C_(35)^+) n-alkanes of high-waxy condensate and its source kitchen orientation in the Qianmiqiao burial-hill zone, Bohai Gulf Basin
High molecular weight (C+35) n-alkanes of high-waxy condensate and its source kitchen orientation in the Qianmiqiao burial-hill zone, Bohai Gulf Basin作者机构:Key Laboratory of Petroleum Accumulation Mechanism of the Ministry of EducationUniversity of PetroleumBeijing 102249China Guangzhou Institute of GeochemistryChinese Academy of SciencesGuangzhou 510640China Geological Research InstituteDagang Oilfield(Group)Co.Ltd.Tianjin 300280China
出 版 物:《Science China Earth Sciences》 (中国科学(地球科学英文版))
年 卷 期:2004年第47卷第3期
页 面:255-264页
学科分类:070704[理学-海洋地质] 0709[理学-地质学] 07[理学] 0707[理学-海洋科学]
基 金:This study was supported by the National Natural Science Foundation of China (NSFC No. 40172056) the Research Found for the Doctoral Program of High Education (RFDP No. 2000042506)
主 题:Qianmiqiao burial-hill high temperature gas chromatography (HTGC) high-waxy condensate high molecular weight (HMW) n-alkanes.
摘 要:The high-waxy condensate in the Qianmiqiao Ordovician burial-hill zone, Bohai Gulf Basin, North China has been investigated by way of high temperature gas chromatography. As high-mature oil, its high molecular weight wax fraction is mainly composed of C35—C69 n-alkanes with CPI37—55 values of 0.94—1.10. On conditions that core-drilling of source rocks was limited and the exact location of source kitchen is still uncertain in the region, it is inferred that the ori-entation of main source kitchen for the condensate should be on the east of the burial-hill zone, i.e. from the direction of Qikou Sag, according to oil-oil correlation between the condensate and surrounding high-waxy oils as well as lateral distribution of the wax content of crude oils. In addi-tion, it is also further confirmed that the oil filling direction for this condensate reservoir is from NE to SW, i.e. from wells BS-4, through BS-7, to BS-8 based on the analyses of 9 maturity and 3 pyrrolic N-compound parameters.