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SOURCE ROCK MATURATION AND PETROLEUM<br />

GENERATION AND MIGRATION MODELING OF THE<br />

LEVANTINE BASIN, OFFSHORE LEBANON:<br />

AN INTEGRATED APPROACH<br />

S. Bou Daher, R. Littke, F. H. Nader<br />

04.07.2012 Samer Bou Daher Beirut


Outline<br />

• Project Objectives<br />

• Approach <strong>and</strong> methods<br />

• Preliminary results<br />

• Ongoing work<br />

04.07.2012 Samer Bou Daher Beirut


• Major gas discoveries in the southern Levantine Basin<br />

• Hydrocarbon seeps onshore <strong>and</strong> offshore<br />

• Onshore <strong>source</strong> <strong>rock</strong> analogues<br />

OOne or more working ki <strong>petroleum</strong> l systems<br />

Source <strong>rock</strong>s? k Maturity? Quality? l Distribution? b<br />

North vs. South?<br />

04.07.2012 Samer Bou Daher Beirut


• Mj Major Objectives: Obj i<br />

– 3D <strong>petroleum</strong> system model that integrates <strong>source</strong> <strong>rock</strong><br />

characterization <strong>and</strong> distribution with the evolution <strong>and</strong><br />

filling of the structurally complicated Levantine Basin,<br />

offshore Lebanon<br />

– The model will simulate the distribution of gas <strong>and</strong> oil<br />

accumulations derived from <strong>source</strong> <strong>rock</strong>s, , whose<br />

characteristics could be inferred from field sampling <strong>and</strong><br />

geochemical analyses.<br />

04.07.2012 Samer Bou Daher Beirut


Studying the potential <strong>source</strong> <strong>rock</strong>s <strong>and</strong> assessing their<br />

efficiency using modern geochemical <strong>and</strong> optical methods:<br />

• TOC TOC, TIC TIC, S<br />

• Rock‐Eval<br />

• GC GC, GC GC‐MS MS<br />

• Oxygen <strong>and</strong> Carbon isotope analyses<br />

• Kinetics of f Hydrocarbon d b Generation<br />

• Microscopy (VRr, Fluorescence, SEM)<br />

04.07.2012 Samer Bou Daher Beirut


DIONISOS<br />

KINE 3D<br />

S<strong>and</strong> Box<br />

R. Ghalayini<br />

N. Hawie<br />

INTEGRATED GEOMODEL<br />

TEMIS S. Bou Daher<br />

04.07.2012 Samer Bou Daher Beirut


•Source potential?<br />

•Depositional Depositional environment? Oxic? Anoxic?<br />

•Maturity?<br />

04.07.2012 Samer Bou Daher Beirut


Preliminary results<br />

(Bh 8) (Bh 3)<br />

04.07.2012 Samer Bou Daher Beirut


04.07.2012 Samer Bou Daher Beirut


04.07.2012 Samer Bou Daher Beirut


(Peters, 1986)<br />

04.07.2012 Samer Bou Daher Beirut


04.07.2012 Samer Bou Daher Beirut


04.07.2012 Samer Bou Daher Beirut


Senonian (Chekka<br />

North Lebanon) )<br />

• Pr/Ph = 0.88<br />

• P/Ph Pr/Ph = 0.93 093<br />

< 1<br />

»»» dysoxic<br />

Senonian (Hasbaya<br />

South Lebanon): )<br />

• TOC= 10%<br />

• Pr/Ph = 0.55<br />


Lower Campanian (North Lebanon)<br />

04.07.2012 Samer Bou Daher Beirut


Conclusions:<br />

Very good Senonian <strong>source</strong> <strong>rock</strong>s<br />

Type 1 kerogen (Oil prone) (TOC 1% ─ 5% in the North)<br />

Immature (VRr ̴ 0.35%) → Maximum<br />

Paleotemperature ≈ 40°C<br />

Dysoxic depositional environment (in the North)<br />

Anoxic depositional environment (in the South)?<br />

Deeper?<br />

04.07.2012 Samer Bou Daher Beirut


Ongoing work:<br />

Complete TOC log of the Chekka Formation in North<br />

Lebanon<br />

More data concerning the depositional<br />

environment<br />

Investigation of the migrabitumen in the Chekka<br />

FFormation i iin NNorth hLb Lebanon (Mi (Microscopy,<br />

Biomarkers analysis…)<br />

Submitting Submitting a paper to peer reviewed international<br />

journal<br />

04.07.2012 Samer Bou Daher Beirut


Thank you for your attention<br />

04.07.2012 Samer Bou Daher Beirut

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