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Relevant bibliographies by topics / Gongila Formation

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Academic literature on the topic 'Gongila Formation'

Author: Grafiati

Published: 3 June 2025

Last updated: 31 July 2025

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Journal articles on the topic "Gongila Formation"

1

Mafimisebi, Peter, Grace Martins, Alex America, and Bidemi Ehimentan. "MINERALOGY AND GEOCHEMISTRY ASSESSMENT OF THE CRETACEOUS SEDIMENTS IN KANADI-1 WELLS, BORNU BASIN FORMATION, NORTH-EASTERN NIGERIA." International Journal Of Trendy Research In Engineering And Technology 08, no. 06 (2024): 62–71. http://dx.doi.org/10.54473/ijtret.2024.8608.

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Mineralogical and Geochemical prospect were used to evaluate the Cretaceous and Tertiary sediments in the Bornu Basin of northeastern Nigeria, particularly those found in Kanadi-1 Wells, seeks to gain insight into their origins and how they were deposited. The Bima Sandstone Formation, the sandy-shale Gongila Formation, and the clayeyshaley Fika Formation, are mainly composed of around 35-58% quartz and up to 50% kaolinitic clay. Notably, the quantity of quartz decreases steadily across the stratigraphic sequence. The base of the Bima Sandstone Formation is characterized by its abundance of ar

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Imagbe, O. L., R.M Piwuna, and W.E Egbon. "PRELIMINARY ASSESSMENT OF THE RARE EARTH ELEMENT COMPOSITION OF SHALES OF THE GONGILA FORMATION, GONGOLA BASIN NIGERIA." Continental J. Earth Sciences 5, no. 1 (2017): 14–19. https://doi.org/10.5281/zenodo.833380.

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This preliminary study was carried out on the Shales of the Cenomanian-Turonian sedimentary sequence representing the Gongila Formation of the Gongola Basin as exposed in the Ashaka Cement quarry in Gombe, northeastern Nigeria. A total of ten shale samples were collected from the outcropping sections, out of which five representative samples were subjected to instrumental Neutron Activation Analytical (INAA) methods. The results of the analysis of the shale samples shows the average composition values; La (57),Ce (89.4), Nd (34), Sm (6.94), Eu (1.52),Tb (0.66),Lu (0.42).This result however sho

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3

Ali, S., and K. Mosto-Onuoha. "Assessment of the interval heat flow and thermal resistance at the Faltu-1 well, Borno basin, NE Nigeria." Global Journal of Pure and Applied Sciences 27, no. 2 (2021): 153–69. http://dx.doi.org/10.4314/gjpas.v27i2.8.

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The heat flowing through horizons in the Faltu-1 well, Borno Basin, NE Nigeria was calculated from their thermal conductivities and geothermal gradients with the aim of determining whether or not it is uniform, and if not, the depths where it is diverted, and the possible heat diversion process. The interval heat flow was assessed to be non-uniform. While fluid convection is adjudged to be the major heat diversion mechanism within the Chad Formation with minor heat refraction, the reversed is adjudged to be the situation for the underlying Kerri Kerri Formaton within which increasing sand cont

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4

B., Shettima 1., D. Adams 1. F., I. Haruna 2. A., I. Goro 3. A., and Bukar 1. M. "GEOCHEMICAL FACIES OF THE TURONIAN GONGILA FORMATION, BORNU (CHAD) BASIN, NIGERIA: IMPLICATION FOR PROVENANCE, PALEOCLIMATE AND PALEOWEATHERING CONDITIONS." International Journal of Research - Granthaalayah 6, no. 4 (2018): 144–56. https://doi.org/10.5281/zenodo.1242621.

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Geochemical evaluation of the Gongila Formation of Bornu (Chad) Basin indicated mineralogical compositions of quartz, feldspar, anatase, gypsum, smectite and kaolinite from XRD analysis. Corresponding major oxides from XRF analysis indicated the dominance of SiO2 with an average of 54.91 wt % followed by Al2O3 with 15.92 wt %. CaO, NaO, K2O, MgO, MnO, Fe2O3 TiO2 and P2O5 occurred with average compositions of 1.87%, 1.02%, 2.15%, 1.17%, 0.06%, 3.04%, 0.03% and 1.52 % respectively. Alteration indexes derivations from these oxides consisting of Chemical Index of Alteration (CIA), Plagioclase Inde

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Shettima, B., F. D. Adams, A. I. Haruna, A. I. Goro, and M. Bukar. "GEOCHEMICAL FACIES OF THE TURONIAN GONGILA FORMATION, BORNU (CHAD) BASIN, NIGERIA: IMPLICATION FOR PROVENANCE, PALEOCLIMATE AND PALEOWEATHERING CONDITIONS." International Journal of Research -GRANTHAALAYAH 6, no. 4 (2018): 144–56. http://dx.doi.org/10.29121/granthaalayah.v6.i4.2018.1637.

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Geochemical evaluation of the Gongila Formation of Bornu (Chad) Basin indicated mineralogical compositions of quartz, feldspar, anatase, gypsum, smectite and kaolinite from XRD analysis. Corresponding major oxides from XRF analysis indicated the dominance of SiO2 with an average of 54.91 wt % followed by Al2O3 with 15.92 wt %. CaO, NaO, K2O, MgO, MnO, Fe2O3 TiO2 and P2O5 occurred with average compositions of 1.87%, 1.02%, 2.15%, 1.17%, 0.06%, 3.04%, 0.03% and 1.52 % respectively. Alteration indexes derivations from these oxides consisting of Chemical Index of Alteration (CIA), Plagioclase Inde

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6

Rebelle, M. "The marine transgression in the Benue Trough (NE Nigeria): a palaeogeographic interpretation of the Gongila Formation." Journal of African Earth Sciences (and the Middle East) 10, no. 4 (1990): 643–55. http://dx.doi.org/10.1016/0899-5362(90)90031-9.

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7

Obi, Gordian Chuks. "Upper Cretaceous Gongila Formation in the Hawal Basin, northeast Benue Trough: a storm and wave dominated regressive shoreline complex." Journal of African Earth Sciences 26, no. 4 (1998): 619–32. http://dx.doi.org/10.1016/s0899-5362(98)00036-0.

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8

Okey, Akpunonu, Eliseus. "Lithostratigraphic Interpretation, Geotemperature Analysis, and Hydrocarbon Windows Determination in Seloken Field, Chad Basin, Northeastern Nigeria." International Journal of Research and Innovation in Applied Science IX, no. VII (2024): 376–89. http://dx.doi.org/10.51584/ijrias.2024.907034.

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The aim of this study is to interpret the lithostratigraphic units, analyze geotemperature and determine the hydrocarbon windows in the Seloken Field. Gamma-ray logs and formation tops were used to interpret the lithostratigraphic units. Corrected bottom hole temperature (BHT) data from the wells were used to calculate the geothermal gradients. A formular was derived from the geothermal gradient equation to analyze the geotemperature. Another formular was derived from the geotemperature equation to obtain the hydrocarbon windows. Five major lithostratigraphic units were interpreted. They are:

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Mijinyawa, A., M. S. Ismail, and A. Moumouni. "Geochemical Characterization of Source Rock and Modeling of Hydrocarbon Generation of the Cretaceous Fika and Gongila Formation in the Chad Basin, North Eastern Nigeria." Research Journal of Applied Sciences, Engineering and Technology 12, no. 10 (2016): 1031–43. http://dx.doi.org/10.19026/rjaset.12.2823.

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10

M., S. CHAANDA, G. OBAJE N., A. LAR U., and MOUMOUNI A. "PETROLEUM GEOCHEMISTRY OF KUCHALLI -1 IN THE NIGERIAN SECTOR OF THE CHAD BASIN." Continental J. Earth Sciences 1 (July 7, 2007): 18–24. https://doi.org/10.5281/zenodo.824275.

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Kuchalli -1 well, one of the twenty-three exploratory oil wells drilled in the Nigerian sector of the Chad Basin penetrated a Cretaceous succession comprising the Bima, Gongila, Fika and Chad formations. Organic geochemical analyses were carried out to assess the source-rock potential of forty (40) selected ditch cuttings. Total Organic Carbon (TOC) content was found to vary between 0.5 – 2.0wt % (moderate to good) at a depth of 1700m and 2300m. Hydrogen Index (HI) values correlated against TOC and T<sub>max </sub>values indicate gas generative potential. Results of the investigation show that

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Book chapters on the topic "Gongila Formation"

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Goro, Isah, Muhammad Abubakar, Nuhu Waziri, Bukar Shettima, and Babangida Jibrin. "Facies Analysis, Sequence Stratigraphy and Hydrocarbon Habitat Prospectivity of the Pindiga Formation and Fika Shale, Gongola Sub-basin, Northern Benue Trough, Nigeria." In Advances in Science, Technology & Innovation. Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-030-72547-1_48.

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"Gongzula Formation." In Geological Formation Names of China (1866–2000). Springer Berlin Heidelberg, 2009. http://dx.doi.org/10.1007/978-3-540-93824-8_2367.

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"Gongcha Group." In Geological Formation Names of China (1866–2000). Springer Berlin Heidelberg, 2009. http://dx.doi.org/10.1007/978-3-540-93824-8_2348.

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"Gongba Conglomerate." In Geological Formation Names of China (1866–2000). Springer Berlin Heidelberg, 2009. http://dx.doi.org/10.1007/978-3-540-93824-8_2343.

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Conference papers on the topic "Gongila Formation"

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Ayinla, A., W. H. Abdullah, Y. Makeen, M. B. Abubakar, and B. M. Sarki Yandoka. "Geochemical and Petrographic Characterization of Sedimentary Facies from Maiganga, Gombe Formation, Gongola Sub-basin, Northern Benue Trough Nigeria." In 79th EAGE Conference and Exhibition 2017. EAGE Publications BV, 2017. http://dx.doi.org/10.3997/2214-4609.201701515.

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Abdulkadir, Usman, Jamaluddeen Hashim, Ajay Kumar, Umar Yau, Akpam Simon, and Adamu Dawaki. "3D Seismic Data Design, Acquisition and Interpretation of Kolmani Exploratory Field, Upper Benue Trough, Gongola Basin; Nigeria." In SPE Nigeria Annual International Conference and Exhibition. SPE, 2021. http://dx.doi.org/10.2118/207118-ms.

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Abstract In an Oil and Gas field development plan, identifying appropriate reservoir location of a field and deciding the best design strategy as well as meeting the economic hydrocarbon viability are imperative for sustainability. 3-Dimensional seismic data have become a key tool used by geophysicists in the Oil and Gas industry to identify and understand subsurface reservoir deposits. In addition to providing excellent structural images, the dense sampling of a 3D survey can sometimes make it possible to map reservoir quality and the distribution of Oil and Gas. Primarily, Seismic data sets

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