Families of reservoired crude oils from the Cangdong Sag, Bohai Bay Basin, China

被引:11
|
作者
Cheng, Xiong [1 ,2 ,3 ]
Mao, Zhichao [4 ]
Mao, Rong [1 ,2 ,5 ]
Li, Zhiquan [5 ]
Guan, Quansheng [6 ]
Chen, Xi [4 ]
机构
[1] China Univ Geosci, Sch Energy Resources, Beijing 100083, Peoples R China
[2] Minist Educ, Key Lab Marine Reservoir Evaluat & Hydrocarbon En, Beijing 100083, Peoples R China
[3] Macquarie Univ, Ctr Marine Res, Dept Earth & Planetary Sci, Sydney, NSW 2109, Australia
[4] Yangtze Univ, Coll Resources & Environm, Wuhan 430100, Hubei, Peoples R China
[5] Univ Alberta, Dept Earth & Atmospher Sci, Edmonton, AB T6G 2E3, Canada
[6] PetroChina, Dagang Oilfield Co, Explorat & Dev Res Inst, Tianjin 300280, Peoples R China
关键词
Crude oil; Biomarker; Source input; Depositional environment; Maturity; Oil-to-oil correlation; PETROLEUM SOURCE ROCKS; PHOTIC-ZONE ANOXIA; ORGANIC-MATTER; DEPOSITIONAL ENVIRONMENT; ISOPRENOID HYDROCARBONS; AROMATIC-HYDROCARBONS; MOLECULAR INDICATORS; BIOLOGICAL MARKERS; BIODEGRADATION; MATURATION;
D O I
10.1016/j.orggeochem.2018.05.008
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The organic geochemistry of 35 crude oils from six oil fields across the Cangdong Sag, Bohai Bay Basin, was characterized and an oil family classification was carried out for the first time. Four oil families were classified based on 18 parameters related to source and depositional environment using hierarchical cluster analysis. The families have broadly similar geochemical characteristics which suggest oils derived from lacustrine source rocks deposited in a reducing environment. Family A has relatively abundant C-27 steranes and C-30 4 alpha-methyl-24-ethylcholestanes, high Pr/Ph, C-22/C-21 tricyclic terpane and C31R/C-30 hopane ratios, and low ETR, C-26/C-25 tricyclic terpane and C35S/C34S homohopane ratios. Family A shows higher thermal maturity than families C and D, but lower than family B. The most distinct feature for Family B is the high gammacerane index; they also show slightly higher C-22/C-21 tricyclic terpane, C31R/C-30 hopane and C-29/C-30 hopane, lower dibenzothiophene/phenanthrene, and higher maturity than the other families. Families C and D oils are low maturity and they are more similar to each other than families A and B based on most biomarker ratios. However, family C can be distinguished from family D by slightly higher C-27/C-29 steranes and C-30 4Me/C-29 steranes C-30 4 alpha-methyl-24-ethylcholestanes/C-29 steranes, and lower C-29 steranes/C-30 hopane ratios. A preliminary oil-source rock correlation suggests that the oil families originated from various intervals having different organofacies within the second member of the Kongdian Formation. Family A is more widespread than the other families, supporting extensive distribution of the source rock. Family B was only found in the southern part of Kongdong slope, which suggests limited geographical distribution of the related source rock. Families C and D show similar geographical distributions and dominate Wangguantun, Shenjiapu and Shenvsi fields, suggesting that the source kitchens are near these regions. (C) 2018 Elsevier Ltd. All rights reserved.
引用
收藏
页码:115 / 125
页数:11
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