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25th International Meeting on Organic Geochemistry IMOG 2011

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O-17<br />

Compositi<strong>on</strong> analysis of individual petroleum inclusi<strong>on</strong>s:<br />

Preliminary applicati<strong>on</strong> in the reservoir-filling history of theTahe<br />

oil field, Tarim Basin, NW China<br />

Weijun Shi 1,2 , Maowen Li 1,2 , Binbin Xi 1,2 , Jin Xu 1,2 , Zhir<strong>on</strong>g Zhang 1,2 , Jianzh<strong>on</strong>g Qin 1,2 ,<br />

H<strong>on</strong>g Jiang 1,2<br />

1 Sinopec Research Institute of Petroleum Explorati<strong>on</strong> and Producti<strong>on</strong>, Beijing, China, 2 Wuxi Institute of<br />

Petroleum Geology, Sinopec Research Institute of Petroleum Explorati<strong>on</strong> and Producti<strong>on</strong>, Wuxi, China<br />

(corresp<strong>on</strong>ding author:shiwj0082@yahoo.com.cn)<br />

Individual hydrocarb<strong>on</strong> fluid inclusi<strong>on</strong>s can be<br />

extracted and verified under microscopic observati<strong>on</strong>,<br />

different types of inclusi<strong>on</strong>s formed at different<br />

diagenetic stages can be then analyzed with a variety<br />

of techniques. This report presents the results of our<br />

recent project that uses an <strong>on</strong>line gas<br />

chromatography-mass spectrometer (GC/MS) to<br />

study the chemical compositi<strong>on</strong>s of hydrocarb<strong>on</strong>s in<br />

individual petroleum inclusi<strong>on</strong>s in carb<strong>on</strong>ate<br />

reservoirs. Because of the small volume and the low<br />

c<strong>on</strong>centrati<strong>on</strong> of hydrocarb<strong>on</strong>s in individual inclusi<strong>on</strong>s,<br />

this work represents a significant technical<br />

breakthrough in the petroleum system study of the<br />

Tarim Basin, NW China..<br />

Tahe oil field is situated in southwest of Arkekule<br />

Uplift, Tarim Basin. Crude oils are produced<br />

dominantly from the Ordovician carb<strong>on</strong>ate reservoirs,<br />

overlain by Triassic-Lower Jurassic strata. Upper<br />

Carb<strong>on</strong>iferous-Dev<strong>on</strong>ian and Upper-Middle Jurassic<br />

strata are absent in the study area. Ordovician<br />

carb<strong>on</strong>ate core samples were collected from eastern<br />

Tahe oil field and analyzed for petroleum inclusi<strong>on</strong>s.<br />

Petroleum inclusi<strong>on</strong>s are extremely abundant in these<br />

samples, occurring mainly in calcite and quartz<br />

cements and calcite vein in carb<strong>on</strong>ate rock matrix.<br />

Coeval aqueous and petroleum inclusi<strong>on</strong>s are readily<br />

identified and distinguished under the microscope by<br />

their fluorescence properties, occurrences and<br />

homogenizati<strong>on</strong> temperatures. Two types of<br />

petroleum inclusi<strong>on</strong>s are identified. The first and<br />

dominant type displays blue fluorescence, and the<br />

homogenizati<strong>on</strong> temperatures of the associated<br />

aqueous inclusi<strong>on</strong>s vary from 74 to 92 ooC. The<br />

sec<strong>on</strong>d type of petroleum inclusi<strong>on</strong>s display yellow<br />

fluoresce, iand variable homogenizati<strong>on</strong> temperatures<br />

from 58℃ to 113℃ .<br />

Laser ablati<strong>on</strong> supports the GCMS analysis of small<br />

samples (< 100 mm). It affords ultra-high sensitivity<br />

and an ability to separately analyse in situ<br />

microscopically discrete morphological entities. The<br />

new laser ablati<strong>on</strong> GCMS facilities equipped with<br />

identical GC inlets have been recently established at<br />

the Wuxi Institute of Petroleum Geology, where the<br />

instrument uses a pulsed 193 nm excimer laser<br />

targeting the analyses of oil bearing inclusi<strong>on</strong>s.<br />

Excimer laser is the most suitable tool to open the<br />

fluid inclusi<strong>on</strong>s hosted in quartz or calcite and the high<br />

performance inlet ensures excellent products transfer<br />

.<br />

Results of our <strong>on</strong>-line GCMS analysis for individual<br />

inclusi<strong>on</strong>s indicate that C4-C30 hydrocarb<strong>on</strong>s are<br />

present, and two types of petroleum inclusi<strong>on</strong>s bear<br />

distinctly different chemical compositi<strong>on</strong>s. The blue<br />

fluorescence inclusi<strong>on</strong>s have higher proporti<strong>on</strong>s of<br />

saturated hydrocarb<strong>on</strong>s and gaseous hydrocarb<strong>on</strong>s,<br />

but lower proporti<strong>on</strong>s of aromatic hydrocarb<strong>on</strong>s than<br />

the yellow fluorescencing inclusi<strong>on</strong>s.. Normal alkanes<br />

in the blue fluorescencing inclusi<strong>on</strong>s show a unimodal<br />

distributi<strong>on</strong>, with the maximum at n-C17, and<br />

those in the yellow fluorescencing inclusi<strong>on</strong>s have<br />

dual modal distributi<strong>on</strong>, maximized at n-C15 and C25.<br />

In general, the yellow fluorescencing inclusi<strong>on</strong>s<br />

c<strong>on</strong>tain much more water soluble aromatic<br />

hydrocarb<strong>on</strong>s than those in the blue <strong>on</strong>es, as<br />

indicated by the ratio of 1,7-dimethylnaphthalene/n-<br />

C14 alkane. TBecause the GC retenti<strong>on</strong> time of both<br />

compounds are similar, their ratio is unlikely to be<br />

affected by sample handling processes. Five samples<br />

were analyzed, and the results show that 1,7-<br />

DMN/nC14 ratios in the yellow fluorescencing<br />

inclusi<strong>on</strong>s are around 3.37, while those in the blue<br />

fluorescencing <strong>on</strong>es are <strong>on</strong>ly 0.46. It is reas<strong>on</strong>able to<br />

infer that the compositi<strong>on</strong> and the formati<strong>on</strong> time are<br />

different for these two types of inclusi<strong>on</strong>s.<br />

On the basis of homogenizati<strong>on</strong> temperatures and<br />

fluorescence, in particular the compositi<strong>on</strong>,it can be<br />

delineated that there were two main stages of the<br />

petroleum-filling in the Tahe oil field. Compared with<br />

the blue fluorescence petroleum inclusi<strong>on</strong>s, the yellow<br />

<strong>on</strong>es have a lower maturity level, which may be<br />

caused by an early hydrocarb<strong>on</strong> charge.<br />

75

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