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MINERALOGICAL, GEOCHEMICAL, MICROMORPHOLOGICAL AND SPECTRAL ANALYSES OF QUARTZ SANDSTONES IN NORTHWEST CHAD BASIN, NIGERIA

Yıl 2019, Cilt: 5 Sayı: 1, 127 - 136, 30.06.2019

Öz

Here, we present quartz sandstone samples observed from widely distributed, white-coloured, uncemented units in and around Matsena village located in northwest of Chad Basin, NE Nigeria. The mineralogical, geochemical compositions and micromorphological characteristics of the quartz sandstones were determined by X-ray diffraction (XRD), X-ray fluorescence (XRF), stereo microscope and scanning electron microscopy (SEM), respectively. The spectral distribution of these lithological units was determined by using Landsat 8 OLI and image enhancement techniques. XRD and XRF analyses reveal that the quartz sandstone samples can be characterized as mature-super mature by their high SiO2 contents. General appearances of the quartz grains under SEM show rounded to sub-rounded and to a lesser extent subangular habits with dish-shaped cavities, V-shaped depressions, mature conchoidal fractures and linear grooves, all of which suggest the mechanical impact on quartz grains from aeolian, fluvial-marine and colluvial environments. 

Kaynakça

  • 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 (CR/05/219N) (Unpublished).[3] Adelana, S.M.A., Olasehinde, P.I., Bale, R.B., Vrbka, P., Edet, A.E., Goni, I.B., 2008, “An overview of the geology and hydrogeology of Nigeria”, In: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.

KUZEYBATI ÇAD HAVZASI, NİJERYA KUVARS KUMTAŞLARININ MİNERALOJİK, JEOKİMYASAL, MİKROMORFOLOJİK VE SPEKTRAL ANALİZLERİ

Yıl 2019, Cilt: 5 Sayı: 1, 127 - 136, 30.06.2019

Öz

Burada, KD Nijerya Çad Havzasının kuzeybatısında yer alan Matsena yerleşimi civarından kuvars kumtaşı örneklerini sunuyoruz. Bu kuvars kumtaşlarının mineralojik, jeokimyasal bileşimi ve mikromorfolojik özellikleri sırasıyla XRD, XRF, stereo mikroskop ve SEM analizleri ile belirlenmiştir. Bu litolojik birimlerin alansal dağılımı Landsat 8 OLI ve görüntü iyileştirme teknikleri ile belirlenmiştir. XRD ve XRF analizleri, kuvars kumtaşı örneklerini, yüksek SiO2 içeriğinden dolayı olgun- ileri olgun olarak karakterize edilebileceğini göstermiştir. Kuvars tanelerinin SEM ile genel görünümleri yuvarlaktan yarı yuvarlak ve daha az oranda yarı köşeli morfolojide; çanak şekilli boşluklu, v şeklinde çukurlu, gelişmiş konkoidal çatlaklı ve lineer çizgili morfolojisini gösterir; bunlar da kuvars taneleri üzerinde mekanik etkinin eoliyen, flüvyal-denizel ve kolüvyal ortamlardan geliştiğini önermektedir.

Kaynakça

  • 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.
Toplam 2 adet kaynakça vardır.

Ayrıntılar

Birincil Dil İngilizce
Konular Mühendislik
Bölüm Makaleler
Yazarlar

Öykü Ataytür 0000-0002-2088-7695

Ceren Küçükuysal 0000-0002-4108-3522

Kemal Zorlu 0000-0003-2111-4659

Aliyu Bashir Albishir Bu kişi benim 0000-0003-1586-8905

Murat Gül 0000-0003-1555-6426

Yayımlanma Tarihi 30 Haziran 2019
Yayımlandığı Sayı Yıl 2019 Cilt: 5 Sayı: 1

Kaynak Göster

APA Ataytür, Ö., Küçükuysal, C., Zorlu, K., Albishir, A. B., vd. (2019). MINERALOGICAL, GEOCHEMICAL, MICROMORPHOLOGICAL AND SPECTRAL ANALYSES OF QUARTZ SANDSTONES IN NORTHWEST CHAD BASIN, NIGERIA. Mugla Journal of Science and Technology, 5(1), 127-136.
AMA Ataytür Ö, Küçükuysal C, Zorlu K, Albishir AB, Gül M. MINERALOGICAL, GEOCHEMICAL, MICROMORPHOLOGICAL AND SPECTRAL ANALYSES OF QUARTZ SANDSTONES IN NORTHWEST CHAD BASIN, NIGERIA. MJST. Haziran 2019;5(1):127-136.
Chicago Ataytür, Öykü, Ceren Küçükuysal, Kemal Zorlu, Aliyu Bashir Albishir, ve Murat Gül. “MINERALOGICAL, GEOCHEMICAL, MICROMORPHOLOGICAL AND SPECTRAL ANALYSES OF QUARTZ SANDSTONES IN NORTHWEST CHAD BASIN, NIGERIA”. Mugla Journal of Science and Technology 5, sy. 1 (Haziran 2019): 127-36.
EndNote Ataytür Ö, Küçükuysal C, Zorlu K, Albishir AB, Gül M (01 Haziran 2019) MINERALOGICAL, GEOCHEMICAL, MICROMORPHOLOGICAL AND SPECTRAL ANALYSES OF QUARTZ SANDSTONES IN NORTHWEST CHAD BASIN, NIGERIA. Mugla Journal of Science and Technology 5 1 127–136.
IEEE Ö. Ataytür, C. Küçükuysal, K. Zorlu, A. B. Albishir, ve M. Gül, “MINERALOGICAL, GEOCHEMICAL, MICROMORPHOLOGICAL AND SPECTRAL ANALYSES OF QUARTZ SANDSTONES IN NORTHWEST CHAD BASIN, NIGERIA”, MJST, c. 5, sy. 1, ss. 127–136, 2019.
ISNAD Ataytür, Öykü vd. “MINERALOGICAL, GEOCHEMICAL, MICROMORPHOLOGICAL AND SPECTRAL ANALYSES OF QUARTZ SANDSTONES IN NORTHWEST CHAD BASIN, NIGERIA”. Mugla Journal of Science and Technology 5/1 (Haziran 2019), 127-136.
JAMA Ataytür Ö, Küçükuysal C, Zorlu K, Albishir AB, Gül M. MINERALOGICAL, GEOCHEMICAL, MICROMORPHOLOGICAL AND SPECTRAL ANALYSES OF QUARTZ SANDSTONES IN NORTHWEST CHAD BASIN, NIGERIA. MJST. 2019;5:127–136.
MLA Ataytür, Öykü vd. “MINERALOGICAL, GEOCHEMICAL, MICROMORPHOLOGICAL AND SPECTRAL ANALYSES OF QUARTZ SANDSTONES IN NORTHWEST CHAD BASIN, NIGERIA”. Mugla Journal of Science and Technology, c. 5, sy. 1, 2019, ss. 127-36.
Vancouver Ataytür Ö, Küçükuysal C, Zorlu K, Albishir AB, Gül M. MINERALOGICAL, GEOCHEMICAL, MICROMORPHOLOGICAL AND SPECTRAL ANALYSES OF QUARTZ SANDSTONES IN NORTHWEST CHAD BASIN, NIGERIA. MJST. 2019;5(1):127-36.

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