Shoreface facies model of Cretaceous Jessu Formation, Yola Sub-basin, Northern Benue Trough, northeast Nigeria: New insights from facies analysis and molecular geochemistry

Sarki Yandoka, Babangida M. and Abdullah, Wan Hasiah and Abubakar, M.B. and Johnson, Howard and Adegoke, Adebanji Kayode and Arabi, A.S. and Bata, Timothy P. and Hassan, Meor Hakif Amir and Mustapha, Khairul Azlan and Usman, Musa Bappah (2019) Shoreface facies model of Cretaceous Jessu Formation, Yola Sub-basin, Northern Benue Trough, northeast Nigeria: New insights from facies analysis and molecular geochemistry. Journal of African Earth Sciences, 152. pp. 10-22. ISSN 1464-343X, DOI https://doi.org/10.1016/j.jafrearsci.2019.01.006.

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Official URL: https://doi.org/10.1016/j.jafrearsci.2019.01.006

Abstract

The Yola Sub-basin in the Northern Benue Trough is a frontier exploration basin in northeastern Nigeria and to date, there is no subsurface data available. The oldest sedimentary unit in the Yola Sub-basin is the Bima Formation, followed by Yolde, Dukul, Jessu, Sekuliye, Numanha and Lamja Formations, ranging in age from Berremian-Aptian-Albian to Santonian. The sediments of Jessu Formation were studied based on facies analysis (lithofacies and palynofacies) and geochemistry (biomarker distribution) with an objective of analysing and interpreting the source input/origin, paleodepositional conditions, paleodepositional environment and to reconstruct depositional and facis model for the studied successions. The study revealed that the sediments were deposited in a distal oxic-suboxic to relatively anoxic shelf (shallow marine) environment with both aquatic,-marine and terrestrially derived source inputs. Depositional framework indicate a progradational wave and storm-dominated shoreface-offshore facies succession, displaying a coarsening upward trend. This represent a regressive shoreface-offshore depositional system, consistent with earlier interpretations that the Cretaceous sediments of Jessu Formation were deposited during a brief regressive phase in the Northern Benue Trough. © 2019 Elsevier Ltd

Item Type: Article
Funders: UNSPECIFIED
Uncontrolled Keywords: Yola Sub-basin; Jessu formation; Offshore; Shoreface; Facies models
Subjects: Q Science > Q Science (General)
Q Science > QE Geology
Divisions: Faculty of Science > Department of Geology
Depositing User: Ms. Juhaida Abd Rahim
Date Deposited: 22 Jan 2020 01:29
Last Modified: 22 Jan 2020 01:29
URI: http://eprints.um.edu.my/id/eprint/23520

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