تعداد نشریات | 161 |
تعداد شمارهها | 6,532 |
تعداد مقالات | 70,504 |
تعداد مشاهده مقاله | 124,122,290 |
تعداد دریافت فایل اصل مقاله | 97,230,074 |
Airborne Geophysical Data Interpretation of Nkalagu and Abakaliki Regions of the Lower Benue Trough, Nigeria: Implication for Mineral Potentiality | ||
فیزیک زمین و فضا | ||
مقاله 2، دوره 48، شماره 4، اسفند 1401، صفحه 21-32 اصل مقاله (1.77 M) | ||
نوع مقاله: مقاله پژوهشی | ||
شناسه دیجیتال (DOI): 10.22059/jesphys.2022.331487.1007368 | ||
نویسندگان | ||
.Ejike K Nnaemeka1؛ .Johnson C Ibuot* 2؛ .Daniel N Obiora3؛ Suleiman Taufiq4 | ||
1Department of Physics and Astronomy, Faculty of Physical Sciences, University of Nigeria, Nsukka, Enugu State, Nigeria. E-mail: ejikekings24@gmail.com | ||
2Corresponding Author, Department of Physics and Astronomy, Faculty of Physical Sciences, University of Nigeria, Nsukka, Enugu State, Nigeria. E-mail: johnson.ibuot@unn.edu.ng | ||
3Department of Physics and Astronomy, Faculty of Physical Sciences, University of Nigeria, Nsukka, Enugu State, Nigeria. E-mail: daniel.obiora@unn.edu.ng | ||
4Department of Science Education, Waziri Umaru Federal Polytechnic, Birnin Kebbi, Kebbi State, E-mail: suleimantaufiq@gmail.com | ||
چکیده | ||
This study was carried out to delineate possible mineralized zones within Nkalagu and Abakaliki by mapping the structural and hydrothermal alteration zones deduced from the available aeromagnetic and aeroradiometric datasets. Magnetic enhancement techniques such as total magnetic intensity (TMI), reduction to the equator (RTE), analytical signal (AS) and center for exploration targeting (CET) were utilized. The Potassium, Thorium, Uranium, ternary image maps and the K/Th ratio map were produced to aid the interpretation process of alteration areas. The results obtained from the analysis of the airborne magnetic data identified and enhanced the magnetic signatures that reflect the structural features (lineament) of the study area, by revealing the structural trends at the ENE-WSW, NE-SW and WNW-ESE as major trends and NNE-SSW, NW-SE, NNW-SSE as minor trends. The analysis of radiometric data revealed the concentrations of Thorium (eTh), Uranium (eU), and Potassium (%K) concentrations, which were used for the classification of the rock types present in the area. These classifications identified intrusions of basically igneous rocks such as granite, gabbro, rhyolite, diabase, and metamorphic rocks such as quartzite and schist. The areas believed to be hydrothermally altered, aligned NW-SW, NNE-SSW, SE, central potions, and NE borders were identified based on the concentration of radioelements, using K/Th ratio and the ternary maps. Hence, the results obtained from the analysis of the two methods mapped geological structures, geological boundaries, and alteration areas that could be target areas of possible mineral deposits. | ||
کلیدواژهها | ||
Aeromagnetic؛ Aeroradiometric؛ Structures؛ Alteration Zones؛ Mineralization | ||
مراجع | ||
Abangwu, J.U., Obiora, D.N., Ibuot, J.C., & Ekwueme, O.U. (2021) Estimation of Curie point depth and geothermal gradient in parts of the Bida Basin. Nigeria. Journal of Environmental Engineering and Science, 17(1), 41-50. doi.org/10.1680/jenes.20.00054. Ajaka, E.O., & Oyetheiemi, E.O. (2010). Suggesting Areas for Detailed investigation of mineral occurrences in Nigeria for national resources database. ARPN Journal of Engineering and Applied Sciences, 5(11), 27-39. Ananaba, S.E. (1991). Dam sites and crustal mega lineaments in Nigeria. ITC Journal, (1), 26-29. Boamah, D. (1993). Application of soil geochemistry to gold exploration in the Birimian rocks of Ghana. Unpublished M.Sc. Thesis, Case study from Demoni/Dankyira area, pp 1-6. Burke, K.C. (1996). The African plate. South African Journal of Geology, 99, 341-409. Burke, K., Dessauvagie, T.F.J., & White Man, A.J. (1971). Opening of the Gulf of Guinea and Geological History of Benue Depression and Niger Delta. Nature Phy. Sci, 233, 51-55. Core, D., Buckingham, A., & Belfield, S. (2009). Detailed structural analysis of magnetic data – done quickly and objectively, SGEG Newsletter. Dickson, B.L., & Scott, K.M. (1997). Interpretation of aerial gamma ray surveys-adding the geochemical factors. AGSO Journal of Australian Geology and Geophysics, 17(2), 187-200. Ekpa, M.M.M., Ibuot, J.C., Okeke, F., & Obiora, D.N. (2020). Investigation of Subsurface Structures within Parts of Niger Delta, Nigeria, Via Aeromagnetic Data. Geological Behavior, 4(2), 66-71. Geosoft Inc. (1996). OASIS Montaj Version 4.0 User Guide, Geosoft Incorporated, Toronto. Goodhope, A., & Luke, M. (2013). Structural interpretation of Abakiliki- Ugep, Using Airborne and Landsat Thematic Mapper (TM) Data. Journal of Natural Science Research, 3(13), 137-148. Hassanein, H.I.E., & Soliman, K.S. (2009). Aeromagnetic Data Interpretation of Wadi Hawashiya Area for Identifying Surface and Subsurface Structures, North Eastern Desert, Egypt. JKAU: Earth Sci., 20(1), 117-139. Holden, E.J., Dentith, M., & Kovesi, P. (2008). Towards the automatic analysis of regional aeromagnetic data to identify regions prospective for gold deposits. Comput. Geosci, 34, 1505-1513. Killeen, P.G. (1979). Gamma-ray spectrometric methods in uranium exploration–application and interpretation, in P.J. Hood, ed., Geophysics and Geochemistry in Search for Metallic Ores: Geological Survey of Canada, Economic Geology Report 31, 163-230. Kuforijimi, O., & Christopher, A. (2017). Assessment of aero-radiometric data of Southern Anambra Basin for the prospect of radiogenic heat production. J. Appl. Sci. Environ. Manag., 21(4), 743-748. Liu, S., & Mackey, T. (1998). Using images in a geological interpretation of magnetic data. AGSO Research Newsletter, 28. Manu, J. (1993). Gold deposits of Birimian greenstone belts in Ghana: Hydrothermal alteration and thermodynamics. Verlag Mainz, Wissenchaftsverlag, Aachen Herstellung: Fotodruck Mainz GmbH Susterfeldstr, 83, 52072 Aachen. Milligan, P.R., & Gunn, P.J. (1997). Enhancement and presentation of airborne geophysical data. AGSO Journal of Australian Geology and Geophysics, 17(2), 63-75. Murat, R.C. (1972). Stratigraphy and Paleogeography of the Cretaceous and Lower Tertiary in Southern Nigeria, (2nd Eds). African Geology. University of Ibadan Press, 251-266. Nwachukwu, S.O. (1972). The tectonic evolution of the southern portion of the Benue Trough, Nigeria. Jour. Min. and Geol., 11, 45-55. Obiora, D.N., Dimgba, B.C., Oha, I.A., & Ibuot, J.C. (2020). Airborne and Satellite Geophysical Data Interpretation of the Gubio Area in the Bornu Basin, Northeastern Nigeria: Implication for Hydrocarbon Prospectivity. Petroleum and Coal, 64(4), 1504-1516. Ofoegbu, C.O. (1985). A review of the geology of the Benue Trough, Nig. Journal of African Earth Science, 3, 293-296. Ofoegbu, C.O. & Onuoha, K.M. (1991). Analysis of magnetic data over the Abakaliki Anticlinorium of the Lower Benue Trough, Nigeria. Marine and Petr. Geol., 8, 174-183. Ofoha, C.C. (2015). Geological interpretations inferred from a high resolution aeromagnetic (HRAM) data over parts of Mmaku and environs, South Eastern, Nigeria. International Journal of Applied Science and Mathematical Theory, 1(4), 1-15. Oha, I.A., Onuoha, K.M., Nwegbu, A.N., & Abba, A.U. (2016). Interpretation of high-resolution aeromagnetic data over Southern Benue Trough, Southeastern Nigeria. Journal of Earth System Science, 125, 369-385. Ola, P.S., Adekoya, J.A., & Olabode, S.O. (2018). Source rock evaluation of the southwest portion of the Bornu Basin, Nigeria: IOSR. Journal of Applied Geology and Geophysics, 6(3), 27-31. Osinowo, O.O., & Taiwo, T.O. (2020). Analysis of high- resolution aeromagnetic (HRAM) data of lower Benue trough, Southeastern Nigeria, for hydrocarbon potential evaluation. Journal of Astronomy and Geophysics, 9(1), 350-361. Opara, A.I., Onyekuru. S.O., Essien, A.G., Onyewuchi, R.A., Okonkwo, A.C., Emberga, T.T., & Nosiri, O.P. (2015). Lineament and Tectonic Interpretation over Abakiliki Area. Evidences from Airborne Magnetic and Landsat ETM Data. International Journal of Research and Innovations in Earth Science, 2(4), 111-121. Ostrovskiy, E.A. (1975). Antagonism of radioactive elements in well rock alteration fields and its use in aero gamma spectrometric prospecting. International Geological Review, 17, 461-8. Rahaman, M.A., Ajayi, T.R., Oshin, I.O., Asubiojo, F.O. (1988). Trace element geochemistry and geotectonic setting of lle-ife schist belts prec. Geol. Of Nigeria, GSN pub. Kaduna, 241-256. Reyment, R.A. (1965). Aspects of Geology of Nigeria, Ibadan University Press, Ibadan. Silva, A.M., Pires, A.C.B., McCafferty, A., Moraes, R.A.V., & Xia, H. (2003). Application of airborne geophysical data to mineral exploration in the uneven exposed terrains of the Rio Das Velhas greenstone belt. Revista Brasileira de Geociências, 33(2), 17-28. Telford, W.M., Geldart, L.P., & Sheriff, R.E. (1990). Applied Geophysics. Cambridge. University Press, second edition. Taufiq, S. Okeke, F.N. Obiora, D.N., & Ibuot, J.C. (2021). Assessment of geothermal potential of parts of Sokoto Basin, Northwest Nigeria using aero-radiometric data. Modeling Earth Systems and Environment, 6. | ||
آمار تعداد مشاهده مقاله: 917 تعداد دریافت فایل اصل مقاله: 620 |