Ratios of low molecular weight alkylbenzenes (C0-C4) in Chinese crude oils as indicators of maturity and depositional environment

被引:14
|
作者
Cheng, Bin [1 ,2 ,3 ]
Wang, Tieguan [1 ,2 ]
Huang, Haiping [3 ,4 ]
Wang, Guangli [1 ,2 ]
Simoneit, Bernd R. T. [5 ]
机构
[1] China Univ Petr, State Key Lab Petr Resources & Prospecting, Beijing 102249, Peoples R China
[2] China Univ Petr, Dept Organ Geochem & Environm Sci, Coll Geosci, Beijing 102249, Peoples R China
[3] Univ Calgary, Dept Geosci, Calgary, AB T2N 1N4, Canada
[4] China Univ Geosci, Sch Energy Resource, Beijing 100083, Peoples R China
[5] Oregon State Univ, Dept Chem, Corvallis, OR 97331 USA
基金
中国国家自然科学基金;
关键词
Alkylbenzenes; GCxGC-TOFMS; Maturity; Depositional environment; 2-DIMENSIONAL GAS-CHROMATOGRAPHY; BOHAI BAY BASIN; PALEOZOIC MARINE PETROLEUM; FLIGHT MASS-SPECTROMETRY; TARIM BASIN; SOURCE ROCKS; BEIBUWAN BASIN; NW CHINA; JIYANG SUPERDEPRESSION; AROMATIC-COMPOUNDS;
D O I
10.1016/j.orggeochem.2015.08.008
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
A total of 37 oils from three basins in China were analyzed using comprehensive two-dimensional gas chromatography coupled to time-of-flight mass spectrometry (GC x GC-TOFMS) to investigate the distributions of low molecular weight (LMW) alkylbenzenes (C-0-C-4). Thermal maturity and depositional environment exert dominant controls on the carbon number and isomer distributions of LMW alkylbenzenes, while secondary alteration, such as biodegradation or evaporative fractionation, cannot be ruled out. With increasing maturity, the relative abundance of C-3 and C-4 decreases while the C-0-C-2 alkylbenzenes increase. Some variations in isomer distributions of C4 alkylbenzenes are also attributed to maturation, as illustrated by ratios of (m- + p-)/o-propyltoluene and (3,5- + 3,4-)/(2,5- + 2,4-ethylxylene). The 1,2,3,5-/1,2,3,4-tetramethylbenzene ratio (TeMBr) is proposed to distinguish oils derived from source rocks formed under anoxic rather than oxic/dysoxic depositional conditions. The data suggest that TeMBr <1.0 indicates anoxia, while TeMBr >1.5 suggests an oxic/dysoxic depositional environment. Quantitative data show that the differences in TeMBr values are mainly due to variable 1,2,3,5-TeMB concentrations, whereas the range of 1,2,3,4-TeMB concentration is relatively constant. 1,2,3,5-TeMB is enriched in oils derived from source rocks deposited under oxic/dysoxic conditions, but depleted in oils from source rocks deposited under reducing conditions. (C) 2015 Elsevier Ltd. All rights reserved.
引用
收藏
页码:78 / 90
页数:13
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