期刊
ORGANIC GEOCHEMISTRY
卷 164, 期 -, 页码 -出版社
PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.orggeochem.2021.104354
关键词
Fluid inclusions; ToF-SIMS; Fluorescence colour; Maturity
资金
- Swedish Research Council [2015-04129]
- Swedish National Space Agency [198/15, 137/19]
- Australian Research Council [DP130102547]
- Swedish Research Council [2015-04129] Funding Source: Swedish Research Council
The fluorescence color and molecular signature of oil inclusions can provide important information on the thermal maturity and fluid migration history. This study used fluorescence microscopy and molecular mass spectrometric analyses to investigate the chemical compositions of oil inclusions. The results show that yellow fluorescing oil inclusions contain more diverse hydrocarbons compared to the white-blue fluorescing oil inclusions. Depth profiles indicate that the white-blue fluorescing oil inclusions have a higher content of volatile components. Chemical ratio analysis suggests that the thermal maturity of the two types of fluorescing oil inclusions is not significantly different.
The fluorescence colour and molecular signature of oil inclusions can provide precious information on the thermal maturity of inclusion oils and the fluid migration history of basins. Here we show how molecular mass spectrometric analyses in combination with fluorescence microscopy can be used to reveal heterogeneities in the chemical compositions of oil inclusions within a micrometer sized quartz crystal. We used time-of-flight secondary ion mass spectrometry (ToF-SIMS) to extract and directly analyse the molecular content of two yellow and two white-blue fluorescing oil inclusions in a single quartz crystal from the Barrandian Basin (Czech Republic). The cyclic ion species detected primarily in the yellow fluorescing oil inclusions likely originate from steranes, hopanes, and other tricyclic and tetracyclic terpanes, whereas these are less abundant in the white-blue fluorescing oil inclusions. Depth profiles of the fluid inclusions indicate that the white-blue fluorescing oil inclusions are emptied faster in the ToF-SIMS instrument, presumably due to a higher content of more volatile components than in the yellow fluorescing oil inclusions. The phenanthrene to dibenzothiophene ratio derived from ToF-SIMS of the four inclusion oils from the Barrandian Basin indicates marine clastic sediments as the source rocks for all the inclusion oils. The phenanthrene to alkylphenanthrene ratio derived from ToF-SIMS indicates no major difference in thermal maturity of the oil in the white-blue and yellow fluorescing oil inclusions. Instead, variation in the chemical content of the trapped oil induced by trapping fractionation may be the key control.
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