Twenty crude oil samples from the Murzuq Basin, SW Libya (A-, R- and I-Fields in Blocks NC115 and NC186) have been investigated by a variety of organic geochemical methods. Based on biomarker distributions (e.g. n-alkanes, isoprenoids, terpanes and steranes), the source of the oils is interpreted to be composed of mixed marine/terrigenous organic matter. The values of the Pr/Ph ratio (1.36–2.1),
... [Show full abstract] C30-diahopane / C29 Ts ratio and diasterane / sterane ratio, together with the low values of the C29/ C30-hopane ratio and the cross-plot of the dibenzothiophene/phenanthrene ratio (DBT/P) versus Pr/Ph ratio in most of oil samples, suggest that the oils were sourced from marine clay-rich sediments deposited in mild anoxic depositional environments. Assessment of thermal maturity based on phenanthrenes, aromatic steroids (e.g. monoaromatic (MA) and triaromatic (TA) steroid hydrocarbons), together with terpanes, and diasterane/sterane ratios, indicates that crude oils from A-Field are at high levels of thermal maturity, while oils from Rand I-Fields are at intermediate levels of thermal maturity. Based on the distributions of n-alkanes and the absence of 25-norhopanes in all of the crude oils analysed, none of the oils appear to have been biodegraded. Correlation of the crude oils points to a single genetic family and this is supported by the stable carbon isotope values. The oils can be divided into two sub-families based on the differences in maturities, as shown in a Pr/nC17 versus Ph/nC18 cross-plot. Sub-family-A is represented by the highly mature oils from A-Field. Sub-family-B comprises the less mature oils from R- and I-Fields. The two sub-families may represent different source kitchens of different thermal maturity or different migration pathways.