Abstract

The source of marine oils from the deep Tarim Basin is still in debate due to several alteration processes of source indicators. A series of trimethyl-alkylbenzenes has been detected in marine oils from this old, composite basin, besides the reported aryl isoprenoids with 2,3,6-trimethyl substitution (AIPs). They are characterized by regular gas chromatography elution pattern, which is similar to that of n-alkylbenzenes, and suggest a strong possibility of n-alkyl side chains. C15 trimethyl-n-alkylbenzenes were synthesized by Friedel–Crafts acylation of trimethylbenzene isomers to determine their structures. Based on the chromatography and mass spectra data and the coinjection of synthesized compounds, this series of compounds has been assigned as the 2,4,5-trimethyl-n-alkylbenzenes that coeluted with 2,3,5-trimethyl-n-alkylbenzenes, and other trimethyl-n-alkylbenzene isomers were also detected. This series of trimethyl-n-alkylbenzene (AAs) shows much higher relative abundances in light and waxy oils than in normal and heavy oils, which is opposite to the variation in relative abundances of aryl isoprenoids. The ratios of these trimethyl-n-alkylbenzenes to the aryl isoprenoids (AA/AIP ratio) generally show a good correlation with the maturity indicators for most of studied oils despite of some outliers (mainly condensates). The pyrolysis of asphaltenes has confirmed these trends. These results support an important control of thermal stress on the molecular compositions of marine oils from the deep Tarim Basin, besides other secondary alteration processes (such as oil mixing and migration fractionation, among others). These factors should be given a full consideration for the source determination of deep and ultradeep oils.

Highlights

  • Aryl isoprenoids (AIPs) with various trimethyl substitution patterns, e.g., 2,3,6, 2,3,4, and 3,4,5-trimethyl, exist in sediments and oils and are thought to be the diagenetic products of pigments of photosynthetic sulfur bacteria or algae [1,2,3,4,5,6,7,8]

  • We have shown that the detected AAs are relatively abundant in light oils, waxy oils, and some normal oils, which is generally in contrast with the variation in relative abundances of AIPs in various types of oils (Figure 1)

  • A series of trimethyl-substituted alkylbenzenes has been detected in various types of marine oils from the Tarim Basin

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Summary

Introduction

Aryl isoprenoids (AIPs) with various trimethyl substitution patterns, e.g., 2,3,6-, 2,3,4-, and 3,4,5-trimethyl, exist in sediments and oils and are thought to be the diagenetic products of pigments of photosynthetic sulfur bacteria or algae [1,2,3,4,5,6,7,8]. Variations in the ratios of these trimethyl-n-alkylbenzenes to AIPs show a similar tendency to that in the ratios of n-alkanes to isoprenoids and the AIR ratio, which has been attributed to the oil maturity effect These results are further supported by an oil asphaltene pyrolysis and reinforce the critical influence of thermal maturity on the source-indicating parameters of deep oils, which is worthy of a full consideration for the oil source determination of this basin

Geological Background
Experimental Techniques
Results and Discussion
Conclusions
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