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BIOSTRATIGRAPHIC STUDIES OF X1 and X2 BOREHOLES ,X-FORMATION, DAHOMEY BASIN NIGERIA
The Biostratigraphic studies were carried out on core samples of XFormation atDahomey Basin was studied and some key evaluations were reached. The Paleocene age was assigned to the XFormation whichExpand
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Surface Geophysics Character of Maastrichtian - Danian Sediments in parts of Udi - Ezeagu Area, Southern Anambra Basin, Nigeria
Safe and sustainable development of groundwater resources is a key element of the Millennium Development Goals (MDGs). Pursuant to this, surface geophysics involving the Vertical Electrical SoundingExpand
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The role of accommodation/sediment supply regime/basin morphology in predictingcoastal depositional style: A sequence stratigraphic framework approach forselected deep wells of oligocene-miocene
The Oligocene – Miocene sediments of Selected Deep wells in Niger Delta is represented by marine strata that were deposited in either fluvial- wave – or tide – influenced environments. The wire lineExpand
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Micro paleontological depth palaeoecology of early miocene sequences andsystems tracts: A case study of A-60 well in Niger Delta Basin Nigeria
High resolution Biostratigraphic analysis of palaeoecology & systems tract using micropaleontological data acquired from Early Miocene sediments of A-60 Well drilled to a total depth of 14,616ft wasExpand
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Paleoenvironmental Indications From Textural Parameters: A Case Study Of The Paleocene To Eocene Sandstones In Some Parts Of Anambra Basin, South-Eastern, Nigeria.
Paleoenvironmental study of Paleocene to Eocene Sandstone in some parts of Anambra Basin was studied using textural parameters, which includes sieve analysis and pebble morphological methods. TheExpand
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Palynofacies And Kerogen Analysis Of Upper Cretaceous (Early Campanian To Maatrichtian) Enugu Shale And Mamu Formation In Anambra Basin, South-Eastern, Nigeria
The palynofacies and kerogen analysis of the Upper Cretaceous units (Campanian-Maastrichtian) of the Anambra Basin, Southeastern Nigeria was carried out in the studied area. Two major palynofaciesExpand
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