Tidal Flat Depositional System of the Cretaceous Yolde Formation of the Gongola Sub-basin Northern Benue trough N. E. Nigeria: Implication for Macro-Tidal Coastline
B. Shettima
Department of Geology, University of Maiduguri, Nigeria.
M. Bukar
Department of Geology, University of Maiduguri, Nigeria.
A. Kuku
Department of Geology, University of Maiduguri, Nigeria.
H. I. Kamale
Department of Geology, University of Maiduguri, Nigeria.
B. Shettima
Department of Geology, University of Maiduguri, Nigeria.
*Author to whom correspondence should be addressed.
Abstract
This research aims to evaluate the facies and facies association of the Yolde Formation at Kware stream in the Gongola Sub-basin of the Northern Benue Trough with objective of characterizing its paleodepositional environment. Six lithofacies consisting of trough crossbedded sandstone facies (St), massive bedded sandstone facies (Sm), planar crossbedded sandstone facies (Sp), ripple laminated sandstone facies (Sr), parallel sandstone facies (Sl) and mudstone facies (Fm) defining its stratal packages were skewed into distinctive assemblages of flaser, wavy and lenticular bedding. This present a fining upward signature with facies association typical of tidal flat system. This is evident of a coastal progradation with sequences reflecting migration of a supra-tidal mudflat over intertidal mixed-flat zone which progressively superposed subtidal sandflats. This is indicative of a coastal shoreline with a relatively progradational phase within the net transgressive regional framework of the Cretaceous Yolde Formation.
Keywords: Yolde formation, depositional environment, Gongola sub-basin, Benue trough, tidal flats