1Omoruyi, S. O.; 2Ebahili, E. O. & 3Selong,
U, E.
1,2Department of Geology,
University of Benin, Benin City, Nigeria
3Department of Geology,
University of Calabar, Calabar, Nigeria
Email: ebahili789@yahoo.com
Corresponding Author: Ebahili, E. O.
ABSTRACT
This study is aimed at using uphole method of seismic refraction
survey to investigate the thickness of the weathering layer as well as the
velocity regimes of the weathering, unconsolidated and consolidated layers in
meter/second (m/s). This was accomplished by using the information on the thickness of the
weathering layer obtained from the uphole survey to plan depth parameter for
high frequency seismic waves (shots) as it applies to 3-D seismic reflection
survey and also carryout static corrections, geometry error (linear move-out)
correction and migration as it applies to 3-D seismic processing. The study was
carried out in Obayantor between Oredo and Ikpoba Okha Local Government Areas,
Edo State. The field equipment set-up in uphole method of seismic refraction
survey consisted of a calibrated hydrophone harness with marine rope in a well
bore filled with water, a recording equipment called OYO Mc Seis version 3.0, a
Master-Slave controlled blaster, a printer and a field battery to power the
equipment was used. While, the processing and interpretation software was
UDYSIS. Fifteen uphole locations were acquired in this study with identity,
A,B,C,D,E,F,G,H,I,J,K,L,M,N and O at different locations throughout the study
area. Rotary drilling method was used to drill to depths of 63m to 66m and
logging was at 60m, 50m, 4om, 30m, 25m, 20m, 15m, 10m, 5m, 3m, 1m and 0m. The
lithologies of the formations showed mainly sand and clay. From this study, the
weathering layer velocity obtained ranged between 318m/s to 606m/s with an
average value of 449m/s. This shows low velocity with which seismic waves are
propagated. The thickness obtained for the weathering layer ranged between 4.2m
to 10.9m with average value of 7m. The velocity of the unconsolidated layer
obtained ranged between 151m/s to 1220m/s with an average value of 1017m/s. The
thickness of the unconsolidated layer ranged between 4.2m to 22.2m with an
average value of 16m. The value of the velocity obtained for the consolidated
layer ranged between 1528m/s to 1950m/s with an average value of 1714m/s.
Keywords: Uphole, Weathered Layer, Hydrophones, Seismic Refraction, consolidated layer