PETROGRAPHIC AND PALYNOLOGICAL ANALYSES OF THE EZE-AKU GROUP IN AKPOHA AND ENVIRONS, SOUTHERN BENUE TROUGH, NIGERIA

Cretaceous sediments outcropped extensively in the Abakaliki sedimentary basin.Petrographic and palynological analyses of selected outcrop samples from Akpoha and environs were carried out, using the conventional method of acid macerationin order to re-establish the depositional history of the sediments in the area and their provenance, establish the age of sediments and reconstruct their paleoenvironments of deposition, and evaluate the hydrocarbon source rock potential. Lithological units encountered include sandstones, shales, mudstones, and limestone. Result from sandstone petrography shows that most of the sandstones in the area were mostly derived from the metamorphic /igneous basement sources, and were deposited in a very low energy environments where sediments are rapidly deposited with little reworking. Palynological investigation revealed a Late Cenomanian Middle Turonian age for the sediments, with the following index sporomorph assemblage: Cretacaeiporitesscabratus, Ephedripitesmulticostatus, Cretacaeiporitesmulleri, Monosulcites sp., Tricolporopollenites sp. and Tricolpites sp. Palynomorphs of environmental value indicated that the sediments in the area were mostly deposited under openmarine condition, with minor terrigenous input. Kerogen examination features mostly the amorphous organic matter (AOM), followed by opaque debris, giving rise to type 11 / type 111 kerogen, which are generally over mature but have potential to generate oil or gas.

[1]  E. O. Igwe,et al.  Field and lithostratigraphic studies of the Eze-Aku Group in the Afikpo Synclinorium, southern Benue Trough, Nigeria , 2016 .

[2]  Omoboriowo,et al.  Palynofacies And Kerogen Analysis Of Upper Cretaceous (Early Campanian To Maatrichtian) Enugu Shale And Mamu Formation In Anambra Basin, South-Eastern, Nigeria , 2013 .

[3]  M. Abubakar,et al.  Late Cretaceous palynostratigraphy in the Gongola Basin (Upper Benue Trough, Nigeria) , 2011 .

[4]  O. Umeji Palynological evidence of the Turunian / Campanian boundary between the Abakaliki and the Anambra basins, as exposed at Leru along the Enugu-Port Harcourt expressway, southeastern Nigeria , 2007 .

[5]  I. Banerjee Storm lag and related facies of the bioclastic limestones of the Eze-Aku Formation (Turonian), Nigeria , 1981 .

[6]  S. W. Petters Stratigraphic Evolution of the Benue Trough and Its Implications for the Upper Cretaceous Paleogeography of West Africa , 1978, The Journal of Geology.

[7]  S. Nwachukwu The tectonic evolution of the the southern portion of the Benue Trough, Nigeria , 1972, Geological Magazine.

[8]  A. J. Moss BED‐LOAD SEDIMENTS , 1972 .

[9]  R. Folk,et al.  Detrital sedimentary rock classification and nomenclature for use in New Zealand , 1970 .

[10]  H. Jeffreys Origin of the Earth , 1952, Nature.

[11]  R. Folk Stages of textural maturity in sedimentary rocks , 1951 .

[12]  P. D. Krynine Arkose deposits in the humid Tropics; a study of sedimentation in southern Mexico , 1935 .

[13]  A. Obasi,et al.  Foraminiferal Biostratigraphic Analysis of the Late Cenomanian – Turonian Eze-Aku Shale in the Afikpo Synclinorium, Lower Benue Trough, Nigeria , 2015 .

[14]  O. J. Ojo,et al.  Depositional Environments, Organic Richness, and Petroleum Generating Potential of the Campanian to Maastrichtian Enugu Formation, Anambra Basin, Nigeria , 2009 .

[15]  M. Ibrahim,et al.  Paleoecology, palynofacies, thermal maturation and hydrocarbon source-rock potential of the Jurassic-Lower Cretaceous sequence in the subsurface of the north Easern Desert, Egypt , 1997 .

[16]  R. Reyment Aspects of the geology of Nigeria : the stratigraphy of the Cretaceous and Cenozoic deposits , 1965 .