DETERMINATION OF THE SEDIMENTOLOGICAL AND GEOCHEMICAL CHARACTERISTICS OF THE SEDIMENT IN THE NIGER DELTA BASIN
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DETERMINATION
OF THE SEDIMENTOLOGICAL AND GEOCHEMICAL CHARACTERISTICS OF THE SEDIMENT IN THE
NIGER DELTA BASIN
CHAPTER ONE
INTRODUCTION
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.
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