SEDIMENTOLOGY AND FORAMINIFERA ABUNDANCE PATTERN OF THE SEDIMENTARY SUCESSION PENETRATED BY THE DRILL IN MF-3 WELL, CENTRAL SWAMP DEPOBELT, NIGER DELTA BASIN, SOUTHERN, NIGERIA.
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Abstract
This study integrates sedimentological and foraminifera analyses of five (5) ditch-cutting samples obtained at 60 ft intervals from depths 11,550 ft to 11,790 ft in the MF-3 Well, located within the Niger Delta Basin. The investigation aimed to study the sedimentology and foraminifera abundance patterns in the well and objectively interpret the lithologic characteristics, foraminifera diversity and abundance, age and depositional environments of the studied interval. Standard sedimentological and micropaleontological techniques were employed to process and examine the samples. Sedimentologic characteristics were determined based on textural parameters such as grain size, lithology, lithofacies, color, angularity, roundness and sorting . Each 20 g sample was soaked, washed, sieved, dried, and examined under a binocular stereo microscope for foraminifera identification and quantitative assessment. The sedimentological analysis revealed intercalating shalysand lithofacies, one (1) lithofacie unit . One (1) hydrocarbon play element (reservoir rock) was delinated in the well section. The associated minerals delineated in the well includes Iron oxide (heamatite), mica, quartz, feldspar, and tourmaline. The shaly sands are fine to medium-grained, moderately sorted, and quartz-rich, organic indicating marine incursions. The foraminifera analysis recovered the following species Hanzawaia strattonii, Ammonia beccarii, Haplophragmoides narivaensis, Cibicorbisinflata, Bolivina scalprata miocenica, Heterolepa pseudungeriana, Spirosigmoilina oligocaenica, Bathysiphon sp, Florilus costiferum (Nonion 4 sp), Trochammina sp, Epistominella vitrea, Valvulineria sp and Uvigerina subperegrina. A Middle to Late Miocene age and paralic to open shallow-marine (inner neritic) paleoenvironments of deposition was assigned to the studied well section
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