Abstract
The present study of the Abu Roash and Bahariya formations in well GPTSW-7 refines our understanding of the subsurface Cretaceous of the north Western Desert of Egypt. Our investigations are based on the palynological analyses of 71 cuttings samples, of which 24 have also been analyzed for geochemistry, in addition to 3 sidewall cores analyzed for vitrinite reflectance (
R
o).
Four palynological zones and three subzones in addition to a poorly fossiliferous interval ranging in age from Coniacian–Santonian to early Cenomanian are proposed. These include a poorly fossiliferous interval (Coniacian–Santonian),
Dinogymnium vozzhennikovae Interval Zone (late to middle Turonian),
Ephedripites ambiguus–
Ephedripites multicostatus–
Foveotricolpites giganteus–
Foveotricolpites gigantoreticultus Assemblage Zone (early Turonian),
Classopollis brasiliensis Interval Zone (late to middle Cenomanian), and
Afropollis jardinus Interval Zone (early Cenomanian). The succeeding subzones are;
Afropollis kahramanensis Interval Subzone,
Elaterosporites klaszii Interval Subzone and
Cretacaeiporites densimurus Interval Subzone, all of early Cenomanian age.
Total organic carbon (TOC) and Rock–Eval pyrolysis and palynofacies analyses indicate that the Bahariya Formation and the Abu Roash G Member are primarily of kerogen III type and hence gas prone, suggesting a strong influence of hydrogen-enriched organic matter. The Abu Roash A, C–E Members may also be gas prone (type III kerogen) and appear to contain highly oxidized terrestrial organic matter. In contrast, the Abu Roash F Member has very high TOC and HI values and contains a very high proportion of amorphous organic matter (AOM) indicating a highly oil-prone facies. While this finding is not unexpected for anoxic black shale, it contrasts with earlier studies that suggest a gas prone nature.
R
o measurements show that the Bahariya Formation represents an immature-early genesis dry gas phase. This is also true for all investigated samples from the Abu Roash and Bahariya formations, based on their low thermal alteration index (TAI).
Quantitative and qualitative analyses of both the palynoflora and palynofacies show that the Abu Roash A and C Members (B is missing), both of Coniacian–Santonian age, represent oxic proximal and distal shelf environment. The Abu Roash D and E Members, dated as Turonian, represent oxic (proximal) shelf, whereas the Cenomanian Abu Roash F Member was deposited in a distal suboxic–anoxic basin. The Cenomanian Abu Roash G Member and the Bahariya Formation were deposited in a shallow marine and shallow marine to fluvio-deltaic setting, respectively.
The Senonian Palmae Province is recognized in the palynoflora by the presence of
Proteacidites,
Auriculiidites reticulatus,
Ariadnaesporites,
Gabonisporis vigourouxii. On the other hand the Albian–Cenomanian Elaterates Province is characterized by the presence of
Steevesipollenites,
Gnetaceaepollenites,
Elaterocolpites,
Elaterosporites,
Elateroplicites,
Senegalosporites,
Sofrepites,
Afropollis and
Cretacaeiporites.