Series-1 (May – June 2026) May – June 2026 Issue Statistics
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Abstract: The natural process of compaction serves as the main diagenesis process which results in reduced porosity and formation of pore systems and improved mechanical properties of sedimentary basins. The process has been identified but scientists have not yet found the particular textural features which control natural geological environment compaction efficiency. The research explores how the compaction characteristics of loose sandy sediments get controlled through the particle size distribution (PSD) and sorting characteristics which develop during their deposition process. The researchers performed standard......
Keywords: sieve analysis, PSD, compaction, sorting
[1].
Akpabio, Idara & Usen, W.S.. (2025). Carbon Sequestration In Sedimentary Formations: A Case Study Of The Niger Delta Basin, Nigeria. World Journal Of Applied Science & Technology. 16. 256-268. 10.4314/Wojast.V16i2.256.
[2].
Mode, Ayonma & Anyiam, Okwudiri & Ngala, EN. (2013). Compaction And Porosity Based Pore Pressure Prediction In The “Cappe Field”, Coastal Swamp Depobelt, Niger Delta, Nigeria. Global Journal Of Geological Sciences. 11. 10.4314/Gjgs.V11i1.6.
[3].
Nabage, N., Maigari, A., Umar, B., Aliyu, A., Kariya, I., Saidu, F., Mohammed, M., Lawal, A., & Aliyu, M. (2024). Compaction-Induced Porosity Loss In The Cretaceous Bima Formation Around Lakwaime And Dogon Dutsi, Yola Subbasin, Northern Benue Trough, NE Nigeria. Dutse Journal Of Pure And Applied Sciences, 10(1b), 231–242. Https://Doi.Org/10.4314/Dujopas.V10i1b.24
[4].
Rice-Birchall, Elliot & Faulkner, D.R. & Bedford, John. (2022). The Effect Of Grain Size And Porosity On The Nature Of Compaction Localisation In High-Porosity Sandstone. Journal Of Structural Geology. 164. 104740. 10.1016/J.Jsg.2022.104740.
[5].
Maju-Oyovwikowhe G. E And Okudibie E. J. (2023). Sedimentological And Petrographic Analysis Of Side Wall Samples From The Niger Delta Basin, Nigeria: Implications For Depositional Environments And Reservoir Quality. Journal Of Energy Technology And Environment, 5(2), 211–227. Https://Doi.Org/10.5281/Zenodo.8026291
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Abstract: The study applies high-resolution aeroradiometric data to map hydrothermal alteration zones for gold exploration and delineated surface geology in parts of the northwest Nigeria schist belts. The work uses eight NGSA radiometric sheets covering parts of Zamfara State and adjoining parts of Sokoto and Kebbi. Processing and map production were completed in Oasis Montaj software, followed by GIS-based interpretation and integration. Individual radioelement maps for %K, eTh, and eU were generated, then three hydrothermal alteration indicators were computed: K/Th ratio, F parameter, and potassium deviation (Kd). A fuzzy logic weighted overlay combined......
Keywords: aeroradiometric mapping, hydrothermal alteration, gold mineralisation, fuzzy logic weighted overlay and schist belts.
[1].
Abaa, S. I. (1983). The Structure And Petrography Of Alkaline Rocks Of The Mada Younger Granite Complex, Nigeria. Journal Of African Earth Sciences, 3, 107-113.
[2].
Ajibade, A. C., Fitches, W. R., And Wright, J. B. (1979). The Zungeru Mylonites, Nigeria: Recognition Of A Major Unit. Revue De Geologie Et De Geographie Physique, 21, 359–363.
[3].
Akame, J. M., Oliveira, E. P., Poujol, M., Hublet, G., And Debaille, V. (2020). LA-ICP-MS Zircon Upb Dating, Luhf, Smnd Geochronology And Tectonic Setting Of The Mesoarchean Mafic And Felsic Magmatic Rocks In The Sangmelima Granite-Greenstone Terrane, Ntem Complex (South Cameroon). Lithos, 372, 105702. Https://Doi.Org/10.1016/J.LITHOS.2020.105702
[4].
Akinlalu, A. A. (2023). Radiometric Mapping For The Identification Of Hydrothermally Altered Zones Related To Gold Mineralization In Ife–Ilesa Schist Belt, Southwestern Nigeria. Indonesian Journal Of Earth Sciences, 3(1), 54-65.
Https://Www.Journal.Moripublishing.Com/Index.Php/Injoes/Article/View/519
[5].
Airo, M.-L. (2002). Aeromagnetic And Aeroradiometric Response To Hydrothermal Alteration. Surveys In Geophysics, 23(4), 273–302. Https://Doi.Org/10.1023/A:1015556614694
