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25th International Meeting on Organic Geochemistry IMOG 2011

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P-086<br />

Migrati<strong>on</strong> tracers reveal l<strong>on</strong>g-range migrati<strong>on</strong> in the summan<br />

explorati<strong>on</strong> area<br />

Khaled Arouri 1 , S K Panda 2 , S A Satti 3 , Y Yang 1<br />

1 EXPEC Advanced Research Center, Saudi Aramco, Dhahran, Saudi Arabia, 2 Research and Development<br />

Center, Saudi Aramco, Dhahran, Saudi Arabia, 3 Area Explorati<strong>on</strong> Department, Saudi Aramco, Dhahran,<br />

Saudi Arabia (corresp<strong>on</strong>ding author:khaled.arouri@aramco.com)<br />

Explorati<strong>on</strong> around the Summan Platform, north of<br />

Saudi Arabia, is progressively extending west and<br />

south. The shift of explorati<strong>on</strong> effort away from the<br />

kitchen, which lies to the north of the Summan<br />

Platform, has increased the risk of charge access to<br />

the prospects further away to the south and west. A<br />

migrati<strong>on</strong> study — based <strong>on</strong> the geochemical<br />

characteristics of oils — can mitigate this risk and<br />

help better understand the migrati<strong>on</strong> extent from the<br />

Late Jurassic kitchen.<br />

Benzocarbazoles<br />

(benzo[a]carbazole/benzo[c]carbazole; BC) have<br />

been suggested as odometers for oil migrati<strong>on</strong> (Larter<br />

et al., 1996). The systematic BC behavior — for Late<br />

Jurassic Arab-A oils from oilfields in the Summan<br />

area — suggests that these accumulati<strong>on</strong>s are<br />

charged via l<strong>on</strong>g-range migrati<strong>on</strong>, rather than multiple<br />

sourcing from different local kitchens. The BC ratio<br />

systematically decreases southwards from Field A to<br />

Field E (Fig. 1), apparently as a resp<strong>on</strong>se to the<br />

increase in migrati<strong>on</strong> distance from a kitchen to the<br />

north. While Field E is believed to be the most distal<br />

oil bel<strong>on</strong>ging to this petroleum system, any traps<br />

(whether structural or stratigraphic) — al<strong>on</strong>g this<br />

north-south trending l<strong>on</strong>g-range migrati<strong>on</strong> pathway —<br />

are high-graded, especially those closer to the entry<br />

point north of Field A.<br />

The reducti<strong>on</strong> in BC ratio with increasing migrati<strong>on</strong><br />

distance is accompanied by a decrease in oil maturity,<br />

with early-generated, lower-maturity oil (Field E) being<br />

the most-fracti<strong>on</strong>ated, shallowest and furthest away<br />

from the source kitchen. This reducti<strong>on</strong> in ratio is also<br />

associated with a clear API gravity gradient across<br />

the basin, together with a gentle compositi<strong>on</strong>al<br />

(molecular and isotopic) gradient, indicative of<br />

increasing c<strong>on</strong>tributi<strong>on</strong> by more mature oil with depth<br />

toward the north (Field A).<br />

L<strong>on</strong>g-range migrati<strong>on</strong> has probably been facilitated by<br />

a displacement (fill-and-spill) mechanism through<br />

intermediary fields al<strong>on</strong>g the migrati<strong>on</strong> route.<br />

Interestingly, the southward migrati<strong>on</strong> effect<br />

manifested at a regi<strong>on</strong>al scale is also evident at a field<br />

scale, where the north of each field c<strong>on</strong>tains its last<br />

charge, whereas the south c<strong>on</strong>tains its migrati<strong>on</strong><br />

fr<strong>on</strong>t. Vertical and lateral compositi<strong>on</strong>al grading in<br />

some Summan fields is likely due to poor mixing of<br />

several viscous charges from a comm<strong>on</strong> carb<strong>on</strong>ate<br />

source. This observati<strong>on</strong> highlights the importance of<br />

interpreting the compositi<strong>on</strong>al grading of reservoirs<br />

within the larger c<strong>on</strong>text of regi<strong>on</strong>al migrati<strong>on</strong> and<br />

regi<strong>on</strong>al compositi<strong>on</strong>al grading.<br />

Reference Cited<br />

Larter, S.R., Bowler, B., Li, M., Chen, M., Brincat, D.,<br />

Bennett, B., Noke, K., D<strong>on</strong>ohoe, P., Simm<strong>on</strong>s, D.,<br />

Kohnen, M., Allan, J., Telnaes, N., Horstad, I., 1996.<br />

Benzocarbazoles as molecular indicators of<br />

sec<strong>on</strong>dary oil migrati<strong>on</strong> distance. Nature 383, 593–<br />

597.<br />

Depth (ft) below sea level<br />

S.L<br />

-2000<br />

-4000<br />

-6000<br />

-8000<br />

-10,000<br />

-12,000<br />

-14,000<br />

S N<br />

E<br />

15<br />

0.28<br />

a c<br />

most-fracti<strong>on</strong>ated<br />

= most-migrated<br />

D<br />

23<br />

0.59<br />

a c<br />

C<br />

26<br />

0.63<br />

a c<br />

~ 200 km<br />

B<br />

32<br />

0.89<br />

decreasing API<br />

decreasing oil maturity<br />

lighter � 13 C updip<br />

similar source signature (carb<strong>on</strong>ate)<br />

a c<br />

decreasing BC ratio<br />

A<br />

33<br />

0.97<br />

a c<br />

least-fracti<strong>on</strong>ated<br />

= least-migrated<br />

API<br />

Kitchen<br />

BC ratio<br />

Figure 1. Oilfield compositi<strong>on</strong>al gradients as a<br />

functi<strong>on</strong> of distance from the kitchen, including:<br />

benzocarbazole (BC) ratio, API gravity, isotope ratios<br />

and maturity versus depth below sea level. The<br />

benzo[a]carbazole (labeled a) is preferentially<br />

removed relative to benzo[c]carbazole (labeled c).<br />

229

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