Paleoenvironmental Analysis and Its Significance in Sedimentology: Case Study of the Conglomerate Facies of the Awi Formation, Calabar Flank, Southeast Nigeria | Chapter 7 | Advances and Trends in Physical Science Research Vol. 2
Pebble morphometry of unbroken
quartz pebbles collected from the basal section of Awi Formation exposed around
Ewen area, southeastern Nigeria was studied for paleoenvironmental
reconstruction. Paleoenvironmental analysis refers to the study or use of
ancient geological materials (rocks) to infer the depositional environment or
setting within which they were deposited. Pebble morphometric analysis has
aided the determination of paleoenvironment during the deposition of Awi
Formation. The depositional processes responsible for shaping the pebbles and
the environment that prevailed during past geological times was characterised.
This involved the measurement of the three orthogonal axes (long, intermediate
and short), determination of their corresponding roundness, flatness indices
and elongation indices for no less than 200 pebbles. The pebbles were selected
from 20 points across four exposed sections of the Awi Formation around Ewen
village. The roundness was determined using the standard roundness chart. The
results show that the pebbles are sub-rounded to sub-angular and predominantly
compact-bladed. The mean values for the following morphometric parameters:
Flatness index, elongation ratio, maximum projection sphericity index and
oblate-prolate (OP) index are 0.57, 0.78, 0.74 and 15.65 respectively. These
values are in agreement with those of modern fluvial pebbles. This result was
integrated with the deductions from bivariate plots of roundness against
elongation ratio and sphericity against OP index, and they all inferred the deposition
of the conglomeratic sandstones in a fluvial setting with subordinate
transitional setting. Fluviatile process with some overlapping littoral
influence has been shown to be responsible for the variation in clast
morphology of the paraconglomerates (matrix-supported) of Awi Formation.
Integrating all observations viz; the sediment stratification and grading style
(fining upwards successions) and the dominant unidirectional nature of the
crudely imbricate pebbles, a typical fluvial setting is inferred. It is
possible that the jointing, faulting, sheeting and/or exfoliation of the rocks
of the Oban Massif, which is believed to be the principal source of the
sediments (provenance), also accounts for the abundance of vein quartz in the
area which was eventually adapted for this study. Within sedimentary settings
as this one with paraconglomerates associated with high energy flux during
deposition and other typical channel lag deposits are locations of good
economic deposits (placer deposits) and in some cases hydrocarbon accumulation.
Therefore, besides the significance for pebble morphometry in deciphering
paleoenvironments, it also gives clues for potential sites of ore bodies and/or
characteristics of some targets for hydrocarbon pools. There are obviously
several methods for paleoenvironmental reconstruction using sediments as
earlier mentioned, grain morphology is one. However, care must be taken when
reconstructing paleoenvironment because the shape of grains is a result of so
many other factors and for effective utilisation, a careful study and
integration of all other parameters are recommended.
Biography of author(s)
Emmanuel Etim Okon
Department of
Geology, University of Calabar, P.M.B. 1115, Calabar, Nigeria.
Romeo
Akombi Ojong
Department of Geology,
University of Calabar, P.M.B. 1115, Calabar, Nigeria.
Read full article: http://bp.bookpi.org/index.php/bpi/catalog/view/25/65/162-1
View Volume: https://doi.org/10.9734/bpi/atpsr/v2
View Volume: https://doi.org/10.9734/bpi/atpsr/v2
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