MINERALOGICAL, GEOCHEMICAL, MICROMORPHOLOGICAL AND SPECTRAL ANALYSES OF QUARTZ SANDSTONES IN NORTHWEST CHAD BASIN, NIGERIA
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- References
- [1] Okosun, E.A., 1995, “Review of the Geology of Bornu Basin”, Journal of Mining and Geology, 31(2), 113-122.[2] MacDonald, A.M., Cobbing, J., Davies, J., 2005, “Developing groundwater for rural water supply in Nigeria: a report of the May 2005 training course and summary of groundwater issues in the eight focus states”, British Geological Survey, 32pp. (CR/05/219N) (Unpublished).[3] Adelana, S.M.A., Olasehinde, P.I., Bale, R.B., Vrbka, P., Edet, A.E., Goni, I.B., 2008, “An overview of the geology and hydrogeology of Nigeria”, In: Adelana, S.M.A.,MacDonald, A. (Eds.), Applied Groundwater Studies in Africa. IAH Selected Papers on Hydrogeology, 13,171-197.[4] Mohammed, Y.B., Tela, B., 2012, “Assessment of Tertiary Sediments of Bornu Basin for Possible Hydrocarbon Reservoir”, Research Journal in Engineering and Applied Sciences, 1(4), 251-257.[5] Olabode, S.O., Adekoya, J.A., Ola, P.S., 2015, “Distribution of sedimentary formations in the Bornu Basin, Nigeria”, Petrol.Explor.Develop., 42(5), 674–682.[6] Van Breemen, O., Hutchinson, J., Bowden, P., 1975, “Age and Origin of the Nigerian Mesozoic Granites: ARb-Sr Isotopic Study”, Contributions to Mineralogy and Petrology, 50 (3), 157-172.[7] Adegoke, A.K., SarkiYandoka, B.M., Abdullah, W.H., Akaegbobi, I.M., 2014, “Molecular geochemical evaluation of Late Cretaceous sediments from Chad (Bornu) Basin, NE Nigeria: implications for paleo depositional conditions, source input and thermal maturation”, Arabian Journal of Geosciences, 8(3), 1591–1609.[8] Ekweozor, C.M., Okosun, J.I., Ekong, D.E.U., Maxwell, J.R., 1979, “Preliminary organic geochemical studies of samples from Niger Delta, Nigeria”, Part 1: Analysis of crude oils for triterpanes. Chem Geol., 27, 11–28.[9] Doust, H., Omatsola, E., 1990, “Niger Delta”, In: Edwards J.D., Santogrossi P.A., (eds) Divergent/passive Margin Basins, AAPG Memoir 48. American Association of Petroleum Geologists, Tulsa, 239–248.[10] Mohamed, A.Y., Pearson, M.J., Ashcroft, W.A., Illiffe, J.E., Whiteman, A.J., 1999, “Modeling petroleum generation in the Southern Muglad rift basin, Sudan”, AAPG Bull., 83(12), 1943–1964.[11] Peters, K.E., Fowler, M.G., 2002, “Applications of petroleum geochemistry to exploration and reservoir management”, Org Geochem., 33, 5–36.[12] Seewald, J.S., 2003, “Organic-inorganic interactions in petroleum-producing sedimentary basins”, Nature, 426,327–333.[13] Obaje, N.G., Wehner, H., Scheeder, G., Abubakar, M.B., Jauro, A., 2004, “Hydrocarbon prospectivity of Nigeria’s inland basins: from the viewpoint of organic geochemistry and organic petrology”, AAPG Bull., 88(3), 325–353.[14] Peters, K.E., Walters, C.C., Moldowan J.M., 2005, “The biomarker guide: biomarkers and isotopes in petroleum exploration and earth history”, second eds, vol 2. Cambridge University Press, Cambridge.[15] Akinlua, A., Ajayi, T.R., Adeleke, B.B., 2007, “Organic and inorganic geochemistry of northwestern Niger Delta oils”, Geochem J., 41,271–281. [16] Google Earth Pro (December 14, 2015). NE Nigeria. 14º 23’22.16’’N 6º23’38.41’’E. Eye alt 3110.03 km. Image Landsat/Copernicus 2018.[17] UNESCO, 1987, Geological map of Africa (1: 5000, 000). UNESCO, Paris.[18] Geological Survey of Nigeria, 1984, “Geological Map of Nigeria 1:2.000000”, Geological Survey of Nigeria, Kaduna.[19] Barber, W., Jones, D.G., 1960, “The geology and hydrology of Maiduguri, Bornu Province”, Record of the Geological Survey Nigeria.[20] Rao, T.C.M., Venkataratnam, L., Rao, K.R., 1980, “Contrast enhancement of landsat data on multispectral data analysis system”, Journal of the Indian Society of Photo-Interpretation and Remote Sensing, 8(2), 27-32.[21] Kalelioğlu, Ö.,Zorlu, K., Kurt, M.A. Gül, M., Güler, C. 2009, “Delineating compositionally different dykes in the Ulukışla basin (Central Anatolia, Turkey) using computer‐enhanced multi‐spectral remote sensing data”, International Journal of Remote Sensing, 30(11), 2997-3011.[22] Inzana, J., Kusky, T., Higgs, G., Tucker, R., 2003, “Supervised classifications of Landsat TM band ratio images and Landsat TM band ratio image with radar for geological interpretations of central Madagascar”, Journal of African Earth Sciences, 37, 59-7.[23] Hunt, G.R., Salisbury, J.W., Lenhoff, C.J., 1973, “Visible and near-infrared spectra of minerals and rocks”, VI. Additional silicates. Modern Geology, 4, 85–106.[24] Hunt, G.R., Ashley, R.P., 1979, “Spectra of altered rocks in the visible and near infrared”, Economic Geology, 74, 1613–1629.[25] Hunt, G.R., 1980, “Electromagnetic radiation: the communication link in remote sensing”, In Siegal, B.S., Gillespie, A.R., (Eds), Remote Sensing in Geology, 5–45 (New York: Wiley).[26] Hunt, G.R., Hall, R.B., 1981, “Identification of kaolins and associated minerals in altered volcanic rocks by infrared spectroscopy”, Clays and Clay Minerals, 29, 76-78.[27] Segal, D.B., 1982, “Theoretical Basis for Differentiation of Ferric-Iron Bearing Minerals, Using Landsat MSS Data”, In Proceedings of the International Symposium on Sensing of Environment, 2nd Thematic Conference, Remote Sensing for Exploration Geology, 6 10December, Fort Worth, TX, vol. II (Ann Arbor, MI: Publications Environmental Research Institute of Michigan), 949–951. [28] Drury, S., 1987, “Image Interpretation in Geology”, London: Allen and Unwin, 243 pp.[29] Sabins, F.F., 1999, “Remote sensing for mineral exploration”, Ore Geo.Rev, 14(3-4), 157–183.[30] Han, T., Nelson, J., 2015, “Mapping hydrothermally altered rocks with Landsat 8 imagery : A case study in the KSM and Snow field zones , northwestern British Columbia”, In: Geological Fieldwork 2014, British Columbia Ministry of Energy and Mines, British Columbia Geological Survey Paper, 2015-1, pp.103-112.[31] Mwaniki, M.W., Moeller, M.S., Schellmann, G., 2015, “A comparison of Landsat 8 (OLI) and Landsat 7 (ETM+) in mapping geology and visualising lineaments: A case study of central region Kenya”, International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, XL-7/W3, 897–903.[32] Brindley, G.W., 1980, “Quantitative X-Ray Analyses of Clays”, In: Brindley, G. W., Brown, G., (Eds), Crystal Structures of Clay Minerals and Their X-Ray Identification. Mineralogical Society Monograph, 5,411–438.[33] Jackson, M.L., 1979, “Soil Chemical Analysis-Advanced Course, 2nd Edition”, Published by the Author, Madison, Wisconsin, 895.[34] Moore, D.M., Reynolds, J.R., 1989, “X-Ray Diffraction and the Identification and Analysis of Clay Minerals”, Oxford University Press, 332. [35] Thorez, J., 1976, “Practical Identification of Clay Minerals: a handbook for teachers and students in clay mineralogy”, Lelotte, Dison, Belgium.90.[36] Tucker, M., 1988, “Techniques in Sedimentology”, Blackwell Scientific Publications, 394.[37] Moore, D.M. Reynolds, R.C., 1997, “X-ray diffraction and identification and analysis of clay minerals”, Oxford University Press, 135, 819-842.[38] Welton, J.E., 2003, “SEM Petrology Atlas. Methods in Exploration”, Series No. 4, Pub. Amer. Aso. Petro. Geol., 237.[39] Tadeusz, S., Rybka, R.S., Woronko, B., 2009, “Upper Pleistocene and Holocene deposits at Starunia paleontological site and vicinity (Carpathian region, Ukraine)”, Anneles Societatis Geologorum Poloniae, 79(3), 255-278.[40] Al-Dousari, A.M., Al-Hazza, A., 2013, “Physical properties of Aeolian sediments within major dune corridor in Kuwait”, Arabian Journal of Geosciences, 6(2), 519–527.[41] Calvo, F.R., Sánchez, J., Acosta, A., Wolf, D., Faust, D., 2016, “Granulometrical, mineralogical and geochemical characterization of loess deposits in the Tajo Basin”, Quaternary International, 407, 14–28.[42] Újvári, G., Kok, J. F., Varga, G., Kovács, J., 2016, “The physics of wind-blown loess: Implications for grain size proxy interpretations in Quaternary paleoclimate studies”, Earth-Science Reviews, 154, 247–278.jo[43] Pavelić, D., Kovačić, M., Banak, A., Jiménez-Moreno, G., Marković, F., Pikelj, K., Vranjković, A.,Premužak, L.,Tibljaš,D.,Belak, M., 2015, “Early Miocene European loess: A new record of aridity in southern Europe”, Geological Society of America Bulletin, 128(1-2), 110-121.[44] Kleesment, A., 2009, “Roundness and surface features of quartz grains in Middle Devonian deposits of the East Baltic and their palaeo geographical implications”, Estonian Journal of Earth Sciences, 58(1), 71-84.[45] Ali, A.M., Padmanabhan, E., Baioumy, H., 2018, “Incorporation of silica into the goethite structure: a microscopic and spectroscopic study”, ActaGeochimica, 37(6), 911-921.[46] Obaje N.G., 2009, “The Bornu Basin (Nigerian Sector of the Chad Basin). In: Geology and Mineral Resources of Nigeria”, Lecture Notes in Earth Sciences, vol 120. Springer, Berlin, Heidelberg.[47] Platias, S., Vatalis, K.I., Charalampides, G., 2014, “Suitability of Quartz Sands for Different Industrial Applications”, Procedia Economics and Finance,14,491-498.
Ayrıntılar
Birincil Dil
İngilizce
Konular
Mühendislik
Bölüm
Araştırma Makalesi
Yazarlar
Öykü Ataytür
*
0000-0002-2088-7695
Türkiye
Ceren Küçükuysal
0000-0002-4108-3522
Türkiye
Kemal Zorlu
0000-0003-2111-4659
Türkiye
Aliyu Bashir Albishir
Bu kişi benim
0000-0003-1586-8905
Türkiye
Murat Gül
0000-0003-1555-6426
Türkiye
Yayımlanma Tarihi
30 Haziran 2019
Gönderilme Tarihi
25 Şubat 2019
Kabul Tarihi
9 Haziran 2019
Yayımlandığı Sayı
Yıl 2019 Cilt: 5 Sayı: 1