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25th International Meeting on Organic Geochemistry IMOG 2011

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P-275<br />

Aromatic hydrocarb<strong>on</strong>s in oils from cambrian and precambrian<br />

deposits (East Siberia, Russia)<br />

Alexandra Akhmedova 1 , Olga Serebrennikova 2 , Olga Shiganova 1<br />

1 Siberian Research Institute of Geology, Geophysics and Mineral Resources, Novosibirsk, Russian<br />

Federati<strong>on</strong>, 2 Institute of Petroleum Chemistry, SB RAS, Tomsk, Russian Federati<strong>on</strong> (corresp<strong>on</strong>ding<br />

author:ahmedova-sniiggims@yandex.ru)<br />

Oil fields in the East Siberia are found within<br />

Riphean, Vendian and Cambrian deposits. Typical<br />

oils from three of the main East Siberian oil regi<strong>on</strong>s<br />

(Nepa-Botuobinskaya - NB, Baikitskaya - B and<br />

Katangskaya - K) were investigated in order to get<br />

special characteristics of aromatic HC compositi<strong>on</strong> in<br />

them. The investigated area covers the so called<br />

―gold belt‖ of Lena-Tungusskaya basin.<br />

Oils from 8 areas of Riphean-Vendian-<br />

Cambrian deposits from test and explorati<strong>on</strong> drill<br />

boreholes were investigated. Total c<strong>on</strong>tent of m<strong>on</strong>o-,<br />

bi- and tricyclic aromatic HC, which was detected by<br />

GC-MS technique, relative to the c<strong>on</strong>centrati<strong>on</strong> of nalkanes<br />

fluctuates from 6% up to 34%; it is maximum<br />

(15-34%) in oils from NB regi<strong>on</strong> but it is much lower in<br />

oils from K (5-16%) and in oils from B (6-11%)<br />

regi<strong>on</strong>s. Compounds of benzene, naphthalene (N),<br />

fluorene (F) and phenanthrene (P) types are identified<br />

in investigated oils. M<strong>on</strong>oaromatic HC are<br />

predominating in the major part of oils; but the oil from<br />

Sobinskaya area has 11% of c<strong>on</strong>densed arenes <strong>on</strong>ly<br />

and <strong>on</strong>ly three from oils are the exclusi<strong>on</strong> of this rule;<br />

Ns are predominating in these oils. Comparatively to<br />

all the other aromatic HC, Fs are presented in much<br />

lower c<strong>on</strong>centrati<strong>on</strong>s (not more than 2%). The<br />

c<strong>on</strong>centrati<strong>on</strong> of Ps in the most part of oils is 18-23<br />

relative %.<br />

M<strong>on</strong>oarenes. Homological series of<br />

alkylbenzenes with normal compositi<strong>on</strong> and with <strong>on</strong>e<br />

substituent radical (n-AB) are identified am<strong>on</strong>g<br />

m<strong>on</strong>oarenes; this substituent is usually a linear<br />

aliphatic chain with 10-30 atoms of C (C10-C30). In oils<br />

from NB regi<strong>on</strong> the maximum distributi<strong>on</strong> is <strong>on</strong> C17<br />

and C21, mostly <strong>on</strong> C21. In oils from B regi<strong>on</strong> the main<br />

maximum is <strong>on</strong> C11-C13.<br />

Also isomeric ortho-, meta- and para-<br />

methylalkylbenzenes (MAB), dimethylalkylbenzenes<br />

(DMAB) and trimethylalkylbenzenes (TMAB) were<br />

identified. Phytanilbenzene (PhB, C26) with isoprenoid<br />

aliphatic chain C20 and its methyl- and dimethyl-<br />

substituted homologs were identified in all oils.<br />

DMAB is predominating in the m<strong>on</strong>oarenes<br />

mixture in oils from Riphean deposits; their<br />

c<strong>on</strong>centrati<strong>on</strong> is increasing up al<strong>on</strong>g a stratigraphic<br />

cross-secti<strong>on</strong> while the c<strong>on</strong>centrati<strong>on</strong>s of TMAB are<br />

going down and the c<strong>on</strong>centrati<strong>on</strong>s of MAB and n-AB<br />

are increasing.<br />

Biarenes. Identified biarenes include N, F and<br />

their alkyl-substituted homologs which have up to two<br />

methylene groups (Fs) and up to four methylene<br />

groups (Ns) in their side alkyl chains.<br />

The c<strong>on</strong>tent of appropriate Ns in oils from<br />

Lower Cambrian strata is growing up while the<br />

quantity of methylene groups in side substituents of<br />

aromatic rings is increasing. Going down al<strong>on</strong>g<br />

stratigraphic cross-secti<strong>on</strong> <strong>on</strong>e can find similar<br />

c<strong>on</strong>centrati<strong>on</strong>s of compounds with two (DMN) and<br />

three (TMN) atoms of C in oils from the top of<br />

n<strong>on</strong>segmented Vend-Cambrian Stratum (Usolskaya<br />

Formati<strong>on</strong>); N and methylnaphthalene (MN) have high<br />

relative c<strong>on</strong>centrati<strong>on</strong>s in these oils. TMN is the main<br />

compound in more aged oils. The oils from K regi<strong>on</strong><br />

have the biggest c<strong>on</strong>centrati<strong>on</strong>s of unsubstituted N.<br />

Methylfluorenes (MF) are predominating in Fs<br />

of Riphean oils from B regi<strong>on</strong>. Dimethyl-substituted<br />

fluorenes (DMF) are predominating in oils from more<br />

recent deposits.<br />

Triarenes. P and its alkyl-substituted<br />

homologs with 1-4 atoms of C were identified in<br />

investigated oils. Phenanthrenes with two methylene<br />

groups in the side chains (DMP) are predominating<br />

am<strong>on</strong>g all homologs of phenanthrene in all<br />

investigated oils. Their c<strong>on</strong>centrati<strong>on</strong>s are between 26<br />

and 44 relative %.<br />

Analysis of the data showed that there is a<br />

wide variety of alkyl-substituted benzenes, Ns,<br />

fluorenes and Ps in ancient oils. The highest<br />

c<strong>on</strong>centrati<strong>on</strong>s of these compounds were found in oils<br />

from NB regi<strong>on</strong>. Relative c<strong>on</strong>centrati<strong>on</strong>s of special<br />

types of arenes varies in different oils; but in the most<br />

part of oils alkylbenzenes are the most representative<br />

type of arenes.<br />

408

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