Journal Of Research, Science And Management

 Journal

 GIS Technology In The Selection Of A Waste Disposal Site: A Case Study.

 Atejioye, A.A. And Anifowose, A.Y.B.

 2005

to updated soon

 

 Nil

 Disertations

 Remote Sensing Analysis Of The Ifewara-Zungeru Megalineament In Nigeria

 ANIFOWOSE Adeleye Yekini Biodun

 2004

Ifewara-Zungeru fault constitutes the longest linear feature in the Precambrian basement complex of Nigeria. It is an over 550km-long NNE-SSW trending fault which stretches just east of Ijebu Ode in the south, through Ifewara and Okemesi to the southwestern edge of River Niger around Lafiagi. It reappears beneath the sediments of the Nupe Basin and extends northeastwards for over 300km, through Zungeru (as the Zungeru mylonite) to Kalangai (as the Kalangai Fault). Hitherto, no previous worker on this part of the Nigerian basement complex has looked at this megalinear as a continuous entity. In this study, Landsat, SPOT, and side-looking airborne radar images as well as aerial photographs of the zone traversed by the Ifewara-Zungeru Fault zone were studied. Lineaments extracted from the different images are presented as lineament maps, azimuth frequency/length curves, rose diagrams as well as density and intersection maps. Results from the studies indicate the existence of three general sets of fractures: a NNE-SSW set which corresponds mainly to the trend of the Ifewara-Zungeru Fault; an E-W set which is more or less normal to the orientation of the quartzite bands and is associated with gold mineralization in Ilesa area; and a NW-SE set which is associated largely with migmatites and gneisses. The study has also enabled a comparison of the various remote sensing image types and their usefulness for extracting lithologic and structural information over inaccessible basement terrains. For example, the generally continuous and curvilinear nature of the fault zone was better observed on the Landsat and SLAR images, thereby confirming the versatility of these images in the mapping of regional structures. Results of this study also suggest that the Ifewara-Zungeru fault might have developed as a paratectonic suture during the evolution of the Precambrian basement complex in Nigeria. The existence of such a structure is indicative of probable mineralizations associated with it. This study will also be useful in the evaluation and delineation of groundwater abstraction points over the area covered by the study. Finally, this study asserts a probable rejuvenation of the seemingly dormant fault zone in the future in response to the geodynamics of the earth crust. 

 Nil

 Journal

 Stabilization Of Lateritic Soils As A Raw Material For Building Blocks.

 ANIFOWOSE Adeleye Yekini Biodun

 2002

nil

 

 Journal Of Biological And Physical Sciences,

 Journal

 Geotechnical Appraisal Of The Limestone Deposits In Okeluse-Arimogija Area Of Ondo State, Nigeria: Implications For Industrial Use.

 Odeyemi, I.B. Oyinloye, A.O., Anifowose, A.Y.B,

 2000

soon

 

 Nil

 Conference

 Relevance And Sustainability Of Remote Sensing Education In Nigeria

 ANIFOWOSE Adeleye Yekini Biodun

 1998

nil

 

 Nil

 Journal

 Effect Of Bentonite On The Strength Of Fired Lateritic Soil Blocks. Construction And Building Materials

 ANIFOWOSE Adeleye Yekini Biodun

 1996

nil

 

 Nil

 Technical Papers

 Geological And Geophysical Investigations For Groundwater In The Premises Of The Nigerian Agricultural And Cooperative Bank Limited

 ANIFOWOSE Adeleye Yekini Biodun

 1993

nil

 

 Nil

 Technical Papers

  Mineralogical Analyses Of Barite And Dolomite Samples

 ANIFOWOSE Adeleye Yekini Biodun

 1992

nil

 

 Nil

 Journal

 The Performance Of Some Soils Under Stabilization In Ondo State. Nigeria

 ANIFOWOSE Adeleye Yekini Biodun

 1989

nil

 

 Nil

 Disertations

 An Estimation Of Indirect Tensile And Compressive Strengths Of The Ewekoro Limestone, SW Nigeria.

 ANIFOWOSE Adeleye Yekini Biodun

 1984

nil