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INVESTIGATION FOR GROUNDWATER IN ABUJA TECHNOLOGY VILLAGE, USING VERTICAL ELECTRICAL SOUHDfNG (VES
2008-05-01
The geophysical method of Vertical Electrical Sounding (VES)
using Schlumberger array was used in determining the groundwater
potentials of the Abuja Technology Village, Abuja·
DAKAT LYNDA NANFE
- Bachelors
2010-09-09
The area investigated by this project for Iron is in Nassarawa State, N orth
Central Nigeria. The area is located in Agwada development area of
Kokona Local Government area
ABDULRAHMAN ABDULLAH! MA'ARUF
- Bachelors
LITHO FACIES AND SEDIMENTOLOGICAL ASPECT OF BIMA SANDSTONE UPPER BENUE TROUGH, NIGERIA.
2004-07-01
The 13ima Sandstone comprises the oldest cretaceous sedimentary
;equence in the upper 13enue Trough, which uncomformably overlie the
basement rocks. /\ sequence _,: ;hree fold subdivision has been recognized as ...
RABIU ABDULKARIM
- Bachelors
2009-04-01
The ;;tudy area lies in Bauchi/Gombe States , North Eastern Nigeria within latitudes
I 0° I
USMAN AMINU HUSSAINI
- Bachelors
LITHOFACIES ANALYSIS OF THE YOLDE FORMATION AROUND GAR, SHEET 36 NE, GOMBE STATE, NIGERIA.
2017-02-01
In this study, Lithofacies analysis of the Yolde Formation around Gar, Gombe state
(sheet 36 NE, Nigeria), was carried out from results of the studyof patterns of
lithologies, drainage, facies, ...
TABE, OJAGE JUDE
- Bachelors
2017-01-01
The study area lies between latitudes N l0° 12' 25.0" and El 1° 23' 11.9" and
longitudes NI0° 15' 13" and El 1° 25' 55.3" part of sheet 152 Gombe, ...
SUFYANU YUSUF
- Bachelors
2006-10-01
The Gombe Sandstones is a sequence of est�.rnr!' ,a�d
\ 1 •
detaic Sandstones, Shale, Siltstones and Iron Stones which overlie
the Pindiga, Gongila and Fika Shale Formation in the ...
SAMAILA LAOUALI
- Bachelors
2008-03-01
Studies that involve lithostratigraphy, granulometry and petrography were done on
the Cenomanian Yolde Formation exposed at two localities (along Bambam stream
and the scarf of Chengau hill) in the Yola ...
BABANGIDA MOHAMMED S.Y.D
- Bachelors
2011-09-09
The Maastrichtian Patti Formation is alternating shales, siltstone, claystone and
sandstone that is underlain by Lokoja Sandstone and overlain by Agbaja Ironstone
of southern arm of the Bida Basin
SANUSI MUHAMMED TAOFEEQ
- Bachelors
2008-05-01
Studies of facies chnrnctcrislics, petrography and granulometric anulysis
of lhe slruln of the lithoslrnligrnphic scclion of the Dchn-rulani memher
of Pindiga Formation reconstructed, has revealed six(6) lithofacies
(lithofacies A,B,C,D,E and ...
Lumi Elisha Gwamis
- Bachelors