Abstract

The area of study is a portion of the Greater Ughelli Depobelt in Niger Delta Basin. The main aim of the paper is to interpret the sequence stratigraphy of FX-1 and FX-2 wells by employing data sets from biostratigraphic data and well logs. Standard laboratory techniques were used for data treatment while computer software such as Petrel and StrataBugs were used for data simulation, processing, integration and interpretation. Sedimentology, interpreted gamma ray and resistivity well logs integrated with biostratigraphic data were utilized to define the candidate maximum flooding surfaces and sequence boundaries. The wells have the following distributions of sequences: FX-1 well have five depositional sequences with eight candidate maximum flooding surfaces at depths 10011 ft., 9509 ft., 9437 ft., 6362 ft., 5752 ft., 5507 ft., 5161 ft. and 4816 ft. dated 34.0 Ma, 33.0 Ma, 31.3 Ma, 28.1 Ma, 26.2 Ma, 24.3 Ma, 23.2 Ma and 22.0 Ma and seven candidate sequence boundaries at 9616 ft., 6656 ft., 6116 ft., 5639 ft., 5424 ft., 4859 ft. and 4581 ft. dated 33.3 Ma, 29.3 Ma, 27.3 Ma, 24.9 Ma, 23.7 Ma, 22.2 Ma and 21.8 Ma, respectively. FX-2 well have four depositional sequences, five candidate MFSs were identified at 7764 ft., 7196 ft., 6721 ft., 5862 ft. and 5571 ft. dated 34.0 Ma, 33.0 Ma, 31.3 Ma, 28.1 Ma and 24.3 Ma and five candidate SBs at 6941 ft., 6029 ft., 5688 ft., 5653 ft. and 5542 ft. dated 32.4 Ma, 29.3 Ma, 27.3 Ma, 24.9 Ma and 23.7 Ma respectively. The correlation of the two wells and sequence stratigraphic interpretation is a supplementary understanding of the subsurface geology of the Onshore, western Niger Delta area of Nigeria.
 Keywords: Bio-stratigraphic data, Well logs, Sequence stratigraphy, Well correlation.

Highlights

  • Widely used. Hart, (2005)

  • As posited by Whiteman (1982), the Niger Delta clastic section was formed along the aulacogen that was initially established in the course of the disintegration of the South American and African plates in the Late Jurassic

  • Three hundred and eighty two (382) ditch cutting samples from interval 2900 ft. - 9650 ft. of a total depth of 6750 ft. from FX-2 well, six hundred and seventy eight (678) ditch cutting samples from interval 15 ft. - 10,185 ft. of a total depth of 10,170 ft. from FX-1 well and ASCII data were provided by Nigerian Petroleum Development Company (NPDC) of Nigeria

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Summary

Introduction

Widely used. Hart, (2005). The fundamental unit of sequence stratigraphy is the depositional sequence. It emphasizes phases of deposition and non-deposition (associated with periods of rising and falling of sea level). Several workers such as Evamy et al, (1978); Tuttle, et al, (1999); Weber and Daukoru, (1975); Obaje, (2013); Ojo and Gbadamosi, (2013); Okengwu and Amajor, (2015); Alege, (2017); Ozumba and Amojor (1999); Ajayi and Okosun (2014); Ifeoluwadun and Saka (2018) have worked on the biostratigraphy, sequence stratigraphy, structural geology, sedimentology and petroleum geochemistry of the Niger Delta.

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