Ononiwu et al
Greener Journal of Physical Sciences Vol. 3 (1), pp. 006-018, January, 2013.
ISSN: 2276-7851 © 2011 Greener Journals
Research Paper
Manuscript Number: 110912242
Paleoenviromental and Sequence Stratigraphic Studies of the D7.000 Sand, ‘Eme’ Field, Niger Delta, Nigeria
1Soronnadi-Ononiwu,
G. C, 2Omoboriowo, A.O, Yikarebogha Y3
and Madu
, V.C4
1
Department of Geology, Niger Delta University, Amassoma,
Bayelsa,
Nigeria
2, 3 & 4 Department of Geology, University of Port Harcourt, Port Harcourt, Nigeria
Corresponding Author’s Email: adeboriowo @ yahoo. com, Phone 234-8064364657
Abstract:
This research work focuses attention on the geological
properties of a hydrocarbon bearing in ‘Eme’ field of the
Niger Delta. The environment of deposition is examined and
the type produced as a model of the sub-surface reservoir.
To achieve this, an integrated analysis of cores from wells,
as well as biostratigraphic data and wireline logs of the
D7.000 sand were used for the study. The D7.000 sand of
study comprises one major depositional sequence. It is made
up of upper and lower stratigraphic para-sequence sets. The
upper depositional setting is interpreted as transgressive
sand deposits in an estuarine environment. However, the
lower depositional setting is interpreted as progradational
deposits. Hence, the depositional model interpreted for the
reservoir sand is prograding marine shoreface followed by a
transgressive estuarine setting. This shows that a period of
regression was followed by a transgressive phase which led
to the deposition of the estuarine complexes. From the
petrophysical study carried out through use of composite
logs, amalgamated sand is found to be more porous and more
permeable than the tidal channel. Core analysis revealed the
existence of ten lithofacies. These lithofacies are grouped
into facies association in a vertical sequence with a
genetic significance using primary structures and shape of
wireline logs.
Keywords: sequence, stratigraphy, Niger Delta,
paleoenviromental, Eme, D.7000 sand.
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