Series-1 Jul. – Aug. 2021 Issue Statistics
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Abstract: Background: Oloibiri is a community in Bayelsa State, in the Niger Delta region of Nigeria. The first commercial oil discovery in Nigeria was in the community. Oloibiri oilfield produced oil for 20 years and production finally stopped in 1978 and the field was abandoned. There was growing interest in identifying new petroleum prospects within Bayelsa State, as expressed when the State hosted the National Council on Hydrocarbon Summit in 2020. This research focused on the application of magnetic method in delineation of structures and sediment thickness underlying the area; hence, highlighting the basin's structural and sedimentary endowments favourable for hydrocarbon generation, accumulation and migration in the place. The geologic features that enhanced the drying or accumulation of oil within Oloibiri Area were highlighted in this study......
Key Word: Structural Complexity, Structural Faults, Intrusive Activities, Ferruginization of Sandstone, Sedimentary Thickness.
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[4]. Hailemichael K, Abera A, Shimeles F. (2020). Upward Continuation and Polynomial Trend Analysis as a Gravity Data Decomposition, Case Study at Ziway-Shala Basin, Central Main Ethiopian Rift. Heliyon, vol. 6, Issue 1, pp. 1 – 11. https://doi.org/10.1016/j.heliyon.2020.e03292.
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Abstract: When carrying out the data-acquisition phase of the 4 km2 areal extent VES survey at the southern Phase II Development, Gidan Kwano Campus, Minna, Nigeria, concomitant VES-IP surveys were ignored for the points of Profile 11 because the results of the dual VES-IP surveys for these points already existed in the longitudinal traverse (LT) format beyond the northernmost 21st 2 km linear extent station of the 4 km2 areal extent grid. The aim of this study is to process and interpret the central longitudinal traverse data-field of the 4 km2 VES study at the southern Phase II Development of the Gidan Kwano Campus in order to gain insight into the hydro-centric nature of the material along this mid-profile. The VES survey for the mid-profile of interest in this study was carried out over the spread of P11-1 to P11-34 in no particular order but a survey point being determined by the convenience and logistics of getting to that point on the day of survey. Essentially, the log-log plots show more three-layer geological......
Key Word: traverse; georeferencing; VES; resistivity; psedosection; hydro-centric; groundwater
[1]. Acworth, R.I. (1981). The Evaluation of Groundwater Resources in the Crystalline Basement of Northern Nigeria, PhD Thesis, Univ. of Birmingham.
[2]. Jonah, S.A. (2016C). Analyses of pseudosection specific routes of different orientations of fault-traces to determine groundwater flow pattern at a 4km2 tranche of New Development, Gidan Kwano Campus Phase II, Federal University of Technology, Minna, Nigeria. Journal of Science, Technology, Mathematics, and Education (JOSTMED), 12(3), 9 - 18.
[3]. Jonah, S.A., Akpomie, D.P., Ezekwebekwe, L. O., Isah, E.A., Muhammed, A.N., Momoh, A.A., Okoye, C.K., Okpara, K. K., Oni, N.O., Alade, R. O., Yahaya, G. A., Zubair, R.O., Onoja, E.U., and Daramola, O. (2015A). A dual topographic-petrographic control for a 1km2 VES-IP study completed at the Gidan Kwano Campus Phase II Development, Minna, Nigeria. Journal of Science, Technology, Mathematics, and Education (JOSTMED), 11(3), 65 - 76.
[4]. Jonah, S.A. and Adamu, I.B. (2017B). Extraction of depth-to-basement information from the interpretation of vertical electrical sounding data of Gidan Kwano Campus Phase II, Federal University of Technology, Minna, Nigeria. Journal of Information, Education, Science, and Technology (JIEST), 4(1), 126 - 132.
[5]. Jonah, S.A.and Jimoh, M.O. (2016A). Validity of an empirical rule for delineating aquifer prospects at the Gidan Kwano Campus Development Phase II, Federal University of Technology, Minna, Northcentral Nigeria. Journal of Science, Technology, Mathematics, and Education (JOSTMED), 12(2), 18 - 24..
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Abstract: Morphological, petrological and geochemical variations are used to discern the formation of different types of migmatites and their associated charnockitic rocks which are derived from metasedimentary origin. The study area lies within Bauchi sheet 149 NE. Morphological/field description shows a variation in textural and structural features from metatexite to diatexite to (nebulitic) charnockitic rocks that are dark in colouration due to high quantity of mafic minerals derived from its protolith. The diatexite shows variation from melanocratic to leucocratic containing changes in mineralogy and textures. The charnockite exhibits magmatic foliation which makes it to be metamorphic. Petrographically, the rock mainly composed orthopyroxene, silliminite, quartz, plagioclase, k-feldspar, biotite, muscovite and shows metamorphic imprints in microscopic scale such as undulous extinction in quartz, obliteration in albite twinning. The studied plagioclase are essentially Na-rich, characterized......
Key Word: metasedimentary, migmatite, charnockite, plagioclase, garnet, pyroxene
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