Series-1 (Jul. – Aug. 2021)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.
[1]. Asadi HH, Hale M. (1999). Integrated Analysis of Aeromagnetic, Landsat TM and Mineral Occurrence Data for Epithermal Gold Exploration in Northwest Iran. 13th International Conference on Applied Geologic Remote Sensing, Vancouver. British Columbia.
[2]. Chapin DA, Ander ME. (1999). Exploring for Oil and Gas Traps. In Beaumont EA NH Foster (eds.), American Association of Petroleum Geologists Treatise of Petroleum Geology Handbook.
[3]. Chuks O. (2018). History of the Nigerian Petroleum Industry .Nigeria Oilfields Encyclopedia.
[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.
[5]. Hendra G (2015). Gravity and Magnetics for Hydrocarbon and Geothermal Exploration. Joint Convention Balikpapan.
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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
[1]. Oyawoye, M.O., (1965). Review of Nigerian Pre-cretaceous. In: Reyment, R. A., Aspect of the geology of Nigeria, University of Ibadan Press, pp. 16-21.
[2]. Oyawoye, M.O., (1962). On an Occurrence of Fayalite Quartz Monzonite in the Basement Complex around Bauchi, Northern Nigeria. Geol. Mag. Vol. XCVIII, No. 6.
[3]. Oyawoye, M.O., (1964). The geology of the Nigerian Basement Complex – A survey of our present Knowledge of them. J. Niger. Min. Geol. Metall. Soc., 1, pp. 87-103.
[4]. Oyawoye, M.O. (1972). The Basement Complex of Nigeria. In: Dessauvagie, T.F.J. and Whiteman, A.J. Eds., African Geology, University of Ibadan Press, Ibadan, 67-99.
[5]. Rahaman, M. O., (1988a). Recent Advances in the study of the Basement Complex of Nigeria. In: Oluyide, P. O., Mbonu, W. C., Ogezi, A. E., Egbuniwe, I. G., Ajibade, A. C. and Umeji, A.C., (eds). Precambrian Geology of Nigeria, G.S.N. 11-41.
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Abstract: The study area covers the southern offshore portion within the Gulf of Suez (GS) with a surface area of about 4000 km2. The present work aims to evaluate and outline the subsurface geologic conditions and structural framework controlling the study area. To achieve this aim, subsurface geophysical techniques were carried out on Bouguer gravity map. They indicate that the GS is formed from alternative positive and negative anomalies trending mainly in the NW directions. Sharp positive gravity anomalies are located mainly on the eastern and western shoulders while board negative ones are concentrated at the middle parts. Depth estimation methods were applied to locate the......
Key Word: Gulf of Suez; gravity; geologic structure; data analysis.
[1]. Mckenzie, O.P. and Daves, P., 1970: Plate tectonics of the Red Sea and East Africa, Nature, Vol. 22, pp. 243 - 248.
[2]. Said, R., 1962: The Geology of Egypt. Elsevier Publ. Co., Amsterdam. Oxford and New York, pp. 377.
[3]. Sultan, N. and Schutz, K., 1984: Cross faults in the Gulf of Suez area. EGPC, 7th Explor. Semin., Cairo, pp. 1-15.
[4]. Darwish, M., El-Araby, A., 1993: Petrography and diagenetic aspects of some siliclastic hydrocarbon reservoir in relation to the rifting of the Gulf of Suez, Egypt. Geol. Soc. Egypt., Spec. Publ., No. 1: 155-187.
[5]. Moustafa, A. M., 1976: Block faulting in the Gulf of Suez EGPC., 5th Explor. Semin. Cairo, pp. 19.
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Abstract: Aceh is a province of Indonesia with a high level of earthquake vulnerability. The earthquake that occurred in Pidie Jaya in December 2016 caused psychological shock to the victims. To recover from the psychological shock, they must have resilience. There are some factors that influence the resilience of disaster victims. One of which is religiosity. Being religious is one of the characteristics of Acehnese, and it influences their attitudes and actions in dealing with disasters. This study aims to assess the level of resilience and religiosity of the 2016 Pidie Jaya earthquake victims, find the correlation between resilience and religiosity, and then find the contribution of the religiosity......
Key Word: Disaster, Earthquake, Resilience, Religiosity
[1]. Adami, Ardiman, and Rr Indah Ria Sulisyorini. "Spiritualitas Dan Proactive Coping Pada Survivor Bencana Gempa Bumi Di Bantul." Psikologika: Jurnal Pemikiran dan Penelitian Psikologi 13, no. 25 (2008).
[2]. Adisaputri, Gianisa. "The Role of Religious Beliefs and Practices in Disaster : The Case Study of 2009 Earthquake in Padang City , Indonesia The Role of Religious Beliefs and Practices in Disaster : The Case Study of 2009 Earthquake in Padang City , Indonesia" (2016): 1–84. https://core.ac.uk/download/pdf/80334097.pdf.
[3]. Adiyoso, Wignyo, and Hidehiko Kanegae. "The Preliminary Study of the Role of Islamic Teaching in the Disaster Risk Reduction (A Qualitative Case Study of Banda Aceh, Indonesia)." Procedia Environmental Sciences 17 (2013): 918–927. http://dx.doi.org/10.1016/j.proenv.2013.02.110.
[4]. Affandi, Ghozali Rusyid. "Lnternalisasi Nilai-Nilai Transendensi Untuk Meningkatkan Resilensi Pasca Tsunami Di Aceh: Studi Literatur Melalui Peran Keluarga." Procedia: Studi Kasus dan lntervensi psikologi 3, no. 1 (2015): 29–34.
[5]. Aisha. "Hubungan Antara Religiusitas Dengan Resiliensi Pada Remaja Di Panti Asuhan Keluarga Yatim Muhammadiyah Surakarta." Jurnal 1 (2014): 1–14.