Series-1 (Jan. – Feb. 2021)Jan. – Feb. 2021 Issue Statistics
- Citation
- Abstract
- Reference
- Full PDF
- Index Page
- Cover Paper
Abstract: The seismic noise analysis is very useful tool for characterizing the performance of the existing seismic stations and it should be used as a first step in reducing the noise level in seismic signals. The main indicator of the quality of a seismic station is the level of the noise recorded in the absence of seismic signal. The level of noise recorded on seismometer can be reduced by locating the station away from human activity, selecting good geology and ensuring good seismic vault design and constructed at site, including thermal insulation and excellent ground coupling of broadband seismometer. In the year 1998 an ice free, rocky area on Schimacher Oasis was selected to build the Indian second research station "Maitri" (70°45'52" S and 11°44'03" E) in East Antarctica. The seismic background noise is studied at Maitri broadband seismic station operated in continuous mode till date.......
Keywords: Seismic Noise Analysis, Maitri, human activity, Antarctica, Power Spectral Density (PSD), Probability Density Function (PDF).
[1]. Add el-aziz KhairyAbd el-aal, "Very broadband seismic background noise analysis of permanent good seismic stations", J Seismo (2013) 17:223-237,doi 10.1007/s10950-012-9308-5.
[2]. Satish Saha, "Digital broadband seismograph setup to study the seismicity in Maitri Antarctica region", Journal of applied Geology and Geophysics, doi 10.9790/0990-0403010106
[3]. B. A Wibowo ,N.Heryandoko and Rohadi, "Waveform Spectral Analysis to determining the CTBTO'S seismic stations noise characteristics in Indonesia", The 5th International Symposium on Earthquake and Disaster Mitigation.AIP Conf. Proc 173o: 020007-1-020007-7.doi 10/1063/1/4947375.
[4]. Santosh Kumar, Sumer Chopra,Pallabee Choudhary,A.P.Singh,R.B.S.Yadav and B.K. Rastogi, " Ambient noise levels in Gujarat State (India) seismic network", Geomatics, Natural Hazards and Rish, Vol.3, No.4, November 2012,342-354.
[5]. Satish Saha,R.Vijayaraghavan and Joshi Catherine, " Operation and maintenance of Seismological station at Maitri during 33rd Indian Scientific Expedition to Antarctica, doi 10.13140/RG.2.2.16372.65925.
- Citation
- Abstract
- Reference
- Full PDF
Abstract: Foundation designs planning is very critical in engineering works, therefore geophysical investigation was carried out for foundation design of a proposed Dam at IyahGbede, Ijumu Local Government Area of Kogi State with a view to deduce and enhance the knowledge of the near subsurface integrity of the area for engineering structures.Electrical Resistivity method was adopted to conduct the survey for detail and distinct result. The aim of the exercise was to determine the soil properties of the subsoil layers that constitute the foundation soils and their competence as foundation soils for a dam site establishment. Traverse lines were established along E-W direction and six (6) Vertical Electrical Sounding points (VES) which is one dimensional in prospect, werelaid which to reveal the subsurface property of the area.The VES curves types are AA,AH, HA and KH,which depicts that the investigated site is competent for the proposed dam project.
Keywords: Electrical Resistivity Method, Dam Project, Foundation Design, Geophysical Investigation
[1]. Ajibade, A. C., & Wright, J. B. (1989). The Togo-Benin-Nigeria shield: evidence of crustal aggregation in the Pan-African belt. Tectonophysics, 165(1), 125–129.
[2]. Di, Q. and Wang, M. (2010) Determining areas of leakage in the Da Ye Dam using multi-electrode resistivity. Bulletin of Engineering Geology andEnvironment. 69,105-109
[3]. Grant, F.S. and West, G.F., 1965, Interpretation Theory in Applied Geophysics, McGraw Hill, New York
[4]. Grant NK, Hickman MH, Burkholder FR, Powell JL (1972) Kibaran metamorphic belt in Pan-African domain of West Africa. Nature 238:90–91 Jones, H.A. and Hockey, R.D. (1964): The Geologyof the part of Southwestern Nigeria. GeologicalSurvey Nigeria Bulletin, No 31, Pp. 101.
[5]. Grant, R.W., Housley, R.M., and Geller, S. (1972) Hyperfine interactions of Fe2+ in ilmenite. Physical Review B, 5, 1700–1706..
- Citation
- Abstract
- Reference
- Full PDF
Abstract: A geophysical survey, involving electrical resistivity imaging and magnetic method was carried out for evaluating the cause(s) of the three failed segments along Ikare – Ogbagi highway, southwestern Nigeria. A total of fifty - six magnetic data points, three dipole-dipole resistivity and nine Schlumberger vertical electrical sounding datasets were acquired along three traverses across the failed and stable portions of the road. Results showed two major magnetic responses; high and low zones identified as shallow basement/competent or high magnetized weathering resistant strata and weak zones/low weathering resistant strata respectively. High magnetic amplitudes were observed between 0 – 15 m / 25 - 30 m and low between 15 – 25 m / 30 - 100 m for traverse I; high between 40 -- 50 m with a peak at 45 m position and low between stations 0 - 40 m / 55 - 65 m....
Keywords: Geoelectrical, geological, highway, resistivity, stable, substrate
[1]. Gidigasu, M. D., Geological, Resistivity and Geotechnical properties of the superficial deposit found in Carrighton hill area, unpublished M.Sc, Thesis, and National University of Ireland, Erie, 1977
[2]. Madebors, A. O., Pavement design, guidelines and practice for different geological area in Nigeria, 1983, 290-297.
[3]. Adeyemi, G. O., Highway geotechnical properties of laterite residual soil in Ajebo-Ishara geological transition zone of southwestern Nigeria. Unpublished PhD Thesis, Obafemi Awolowo University, Ile-Ife, Nigeria. 1992, 320-335.
[4]. Oladapo, M. I., Olorunfemi, M. O. and Ojo, J. S., Geophysical investigation of road failure in the basement complex area of southwestern Nigeria. Research Journal of Applied Sciences, 2008, 3(2): 103-112, ISSN 1815-932X
[5]. Ogunribido, T. H. T., Mohammed, M. Z., and Adesuyi, A. R., Effect of Engineering Properties on Pavement Failure in Ogbagi Area, Southwestern Nigeria. Journal of Environment and Earth Science, 2015, 5(4); 39-44,.
- Citation
- Abstract
- Reference
- Full PDF
Abstract: The aim of this research is to estimate the aquifer protective capacity at Odo-Ona Elewe, Ibadan, Nigeria using electrical resistivity method. Ten Vertical Electrical Sounding (VES) data were acquired using Schlumberger Electrode Configuration, the VES Data obtained were interpreted using the Win resist software. The results were analyzed using Dar Zarook parameters and Geoelectric section to identify the aquifer zone of groundwater potentiality and to estimate the aquifer protective capacity of the area. The result of the apparent resistivity measurement and interpretation gave a four layered resistivity structure made up of a top soil, clay/sandy clay, sandy and fresh basement. This study has identified area with good groundwater potential and moderate aquifer protective capacity....
Keywords: Longitudinal Conductance, Transverse Resistance, Tranmisitivity, Aquifer Vulnerability, Vertical Electrical Sounding
[1]. Olorufemi MO, Ojo JS, Akintunde OM (1999). Hydrogeophysical evaluation of the groundwater potential of Akure metropolis, Southwestern Nigeria. J. Min. Geol. 35(2): 207 – 228
[2]. Adeniji A E, Omonona O.V, Obiora D.N. and Chukudebelu J.U. (2014)Evaluation of soil corrosivity and aquifer protective capacity using geoelectrical investigation in Bwaribasement complex area, Abuja J. Earth Syst. Sci. 123, No. 3,
[3]. Henriet JP. 1976. Direct applications of the dar zarrouk parameters in ground water surveys. Geophys Prospect. 24:344–353. doi: 2 doi:10.1111/gpr.1976.24.issue-2.
[4]. Abiola O, Enikanselu PA, Oladapo MI (2009). Groundwater potential and Aquifer protective capacity of overburden units in Ado – Ekiti, Southwestern Nigeria. Int.J. Phy. Sci. 4(3): 120 – 132.
[5]. Zohdy AAR, Eaton GP, Mabey DR (1974). Application of surface geophysics to groundwater investigations: Techniques of water resources investigations of the United Geophysical Survey Book. United States Government Printing Office, Washington DI, P. 116.
- Citation
- Abstract
- Reference
- Full PDF
Abstract: This study was conducted to evaluate the petrophysical parameter of the "Alpha Field" in Niger Delta, Nigeria using well log data. Four wells, namely Well 01, Well 02, Well 03, and Well 04 were studied using a suite of logs comprising of gamma-ray, resistivity, sonic, caliper, density, and neutron logs from the wells in the study area. Schlumberger's Petrel 2013 software was used to analyze the data. Quantitative properties including shale volume, porosity, permeability, water saturation, and hydrocarbon saturation were carried out using the well logs. Intervals with low Gamma-Ray reading relative to the Shale Baseline are interpreted as sand units. Based on this, five sand units, labeled as Dove, Saturn, Jasper, Mars, and Neptune were mapped between the depth of 5600ft and 7100ft across the four.....
Keywords: Alpha Oilfield, Hydrocarbon saturation, Niger Delta, Petrophysical Parameters, and Well Log Analysis.
[1]. Gomez-Rivero, P. (1982). Physical Basis of well logging / Concepts and Techniques in Oil and Gas Exploration Book.
[2]. Asquith, G., and Krygowski, D. (2004). Basic Well Log Analysis. American Association of Petroleum Geologists, pp. 244.
[3]. Asquith, G. B., and Gibson, R. C. (1982). Basic well log analysis for geologists, The AAPG, Houston.
[4]. Darling, T. (2005). Well Logging and Formation Evaluation: Elsevier Inc.
[5]. Ellis, D.V., and Singer, J.M., (2007). Well Logging for Earth Scientists Book: Springer.
- Citation
- Abstract
- Reference
- Full PDF
Abstract: The study was carried out with the aim of interpreting the aeromagnetic data to delineate the sedimentary layer thickness over Northern part of Bida Basin for possible hydrocarbon potential. The study area is bounded by longitude 40 30' to 50 30' N and latitude 90 30' to 100 30'E with an estimated total area of 12100 km2 covering four (4) aeromagnetic sheets of Auna, Kontagora, Kainji and Fashe. The Total magnetic intensity(TMI) map was subjected to the regional-residual magnetic field separation using the upward continuation filter. Subsequently, the residual magnetic field anomaly map was subjected to the estimation of the sedimentary layer thickness using; the Spectral depth analysis, Source parameter imaging (SPI) and Euler deconvolution (ED) methods. However, the Spectral analysis revealed a maximum sedimentary thickness of 3.16 km, SPI method revealed a depth......
Keywords: Total magnetic intensity, Residual magnetic intensity, Sedimentary layer thickness, Spectral analysis, Source parameter imaging, Euler deconvolution and Hydrocarbon.
[1]. Obaje, NG. Geology and Mineral Resources of Nigeria, Lecture Notes in the Earth Science, Springer: Heidelberg. 2009.
[2]. Airo, ML. Application of Aerogeophysical Data for gold exploration: Implications for the central Lapland greenstone belt. 2007.
[3]. Akulga, C. Investigating Gold Mineralization Potentials in Part of the Kibi-Winneba Belt of Ghana using Airborne Magnetic and Radiometric data. unpublished M.Sc. Thesis, Kwame Nkuru University. 2013
[4]. Salako, KA. Depth to Basement Determination Using Source Parameter Imaging (SPI) of Aeromagnetic Data: An Application to Upper Benue Trough and Borno Basin, Northeast, Nigeria. Academic Research International, 2014, 5(3): 74-86.
[5]. Akande, SO,Ojo, OJ, Erdtmann, B D,Hetenyi, M. Paleoenvironments, organic petrology and Rock-Eval studies on source rock facies of the Lower Maastrichtian Patti Formation, Southern Bida Basin, Nigeria. Journal of Africa Earth Science 2005, 41:394–406.
- Citation
- Abstract
- Reference
- Full PDF
Abstract: The ultra-deep sandstone reservoirs of the Cretaceous Bashkiqike Formation in Kelasu structural belt are generally characterized by low resistivity, even lower than the regional standard water resistivity, which makes it more difficult to identify the reservoirs with medium and high resistivity. Therefore, through the comprehensive study of logging, seismic and core analysis data, the three-dimensional distribution characteristics of the low-resistivity gas stratum are clarified, and the low-resistivity gas stratum is divided into thick layer concentration type and thin layer dispersion type according to its development location, and the control factors of the two types of low-resistivity stratum are explored. The results show that the distribution of low-resistivity gas reservoirs is influenced......
Keywords: Low-resistivity gas stratum, Kelasu structural belt, Cretaceous Bashijiqike formation, Ultra-deep reservoir, Main controlling factor.
[1]. Givens W W.A conductive rock matrix model (CRMM) for the analysis of low-contrast resistivity formations [J]. The Log Analyst,1987, 28(2): 138-164.Dore, A G, Barents Sea geology, petroleum resources and commercial potential, Arctic, 48(3), 1995, 207-221.
[2]. LI Mei, LAI Qiang, HUANG Ke, et al. Logging identifi-cation of fluid properties in low porosity and low permeability clastic reservoir: A case study of Xujiahe Fm gas reservoirs in the Anyue gas field, Sichuan Basin[J]. Natural Gas Industry, 2013, 33(6) :34-38.
[3]. CHEN Hua.CHEN Xiaoqiang, SUN Lei, et al. Analysis on genesis of low resistivity layers [J]. Journal of Chongqing University of Science and Technology, 2009.11(4).38-41
[4]. BAO Qiang,ZHANG Ting,ZHANG Xiaodong,et al.Application of logging lithofacies identification technology in Block A of the Right Bank of the Amu-Darya River[J].Natural Gas Industry, 2013. 33(11):51-55.