Determination of the sedimentological and geochemical characteristics of the sediment in the niger delta basin
Table Of Contents
Thesis Abstract
Abstract
The Niger Delta Basin in Nigeria is a significant area for oil and gas exploration, making it crucial to understand the sedimentological and geochemical characteristics of the sediment in this region. This study aimed to determine these characteristics through detailed analysis of sediment samples collected from various locations within the Niger Delta Basin. Sedimentological analysis involved the study of sediment grain size, texture, and sedimentary structures. Grain size analysis was conducted using sieving and sedimentation techniques. The results indicated a predominance of fine to very fine sand in the sediment samples, suggesting a depositional environment with relatively low energy conditions. Textural analysis revealed the presence of clay minerals, indicating a significant contribution from terrestrial sources. Geochemical analysis focused on determining the elemental composition of the sediment samples. X-ray fluorescence (XRF) analysis was employed to quantify major and trace elements present in the samples. The results showed varying concentrations of elements such as silicon, aluminum, iron, and calcium, which are indicative of different sediment sources and weathering processes. The combination of sedimentological and geochemical data provided insights into the depositional environment and provenance of the sediment in the Niger Delta Basin. The fine to very fine sand texture suggests deposition in low-energy environments such as floodplains or estuaries, while the presence of clay minerals points to input from terrestrial sources. The elemental composition further supported these findings, highlighting the influence of both local weathering processes and external sources on the sediment. Understanding the sedimentological and geochemical characteristics of the sediment in the Niger Delta Basin has implications for various industries, including oil and gas exploration, environmental management, and geotechnical engineering. By elucidating the origins and depositional history of the sediment, this study contributes to the broader knowledge of sedimentary processes in deltaic environments and provides valuable information for future research and resource management efforts in the region.
Thesis Overview
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</p><p><strong>INTRODUCTION</strong></p><p>The mineralogical and chemical composition of clastic sedimentary rocks are controlled by various factors, including (1) the composition of their source rocks, (2) environmental parameters influencing the weathering of source rocks (e.g., atmosphericchemistry, temperature, rainfall and topography), (3) duration of weathering (4)transportation mechanisms of clastic material from source region to depocenters, (5)depositional environment (e.g., marine versus fresh water), and (6) post-depositional processes (e.g., diagenesis, metamorphism) (Hayashi et al., 1997). Numerousinvestigations are substantiating the above aspects pertaining to genesis of both ancient andmodern siliciclastic sediments (e.g., Dickenson et al., 1983; Nesbitt and Young, 1982, 1984; Bhatia, 1983; Roser and Korsch, 1988; McCann, 1991; Condie et al., 1992; Condie, 1993; McLennan et al., 1993; Nesbitt et al., 1996; Cullers, 2000; Hessler and Lowe 2006; Nagarajan et al., 2007; Spalletti et al., 2008). Several studies have also been focused on the identification of palaeotectonic settings of provenances based on geochemical signatures of siliciclastic rocks (e.g., Dickinson and Suczek, 1979; Bhatia, 1983; Bhatia and Crook, 1986; Roser and Korsch 1986; McLennan and Taylor, 1991). Among the terrigenous sedimentary rocks, shales are considered to represent the average crustal composition of the provenance much better than any other siliclastic rocks (e.g., McCulloch and Wasserburg, 1978). Shales retain most of the mineral constituents of the source and their bulk chemistry preserves the near-original signature of the provenance and more faithfully reveal palaeoweathering conditions (e.g., Pettijohn, 1975; Graver and Scott, 1995). The present note examines the geochemistry of sediment from part of the subsurface Niger Delta Basin province, attempts to constrain there paleo redox and tectonic setting and provenance. Owing to limitations of analytical facilities, the present work is based on chemical analyses data of major and select trace elements of the investigated sediment of the study area.</p>
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