<?xml version="1.0" encoding="UTF-8"?>
<rss xmlns:dc="http://purl.org/dc/elements/1.1/" version="2.0">
<channel>
<title>HIGH RESOLUTION CALCAREOUS NANNOFOSSILS BIOSTRATIGRAPHY OF THREE WELLS 1, 2 AND 3 IN NORTHWEST OFFSHORE NIGER DELTA, NIGERIA</title>
<link>http://hdl.handle.net/123456789/2138</link>
<description/>
<pubDate>Sun, 05 Apr 2026 23:48:04 GMT</pubDate>
<dc:date>2026-04-05T23:48:04Z</dc:date>
<item>
<title>HIGH RESOLUTION CALCAREOUS NANNOFOSSILS BIOSTRATIGRAPHY OF THREE WELLS 1, 2 AND 3 IN NORTHWEST OFFSHORE NIGER DELTA, NIGERIA</title>
<link>http://hdl.handle.net/123456789/2139</link>
<description>HIGH RESOLUTION CALCAREOUS NANNOFOSSILS BIOSTRATIGRAPHY OF THREE WELLS 1, 2 AND 3 IN NORTHWEST OFFSHORE NIGER DELTA, NIGERIA
COLE, JANET ADERONKE
Over the years, various biostratigraphic approaches (foraminifera, pollen and spores)&#13;
have been used for determining age and biozonation which are useful for exploration&#13;
and production activities in the Niger Delta. However actual age determination and&#13;
refined zonation of the deep offshore Niger Delta area have not been achieved. Hence&#13;
the need to determine the litho-stratigraphic sequence, age of the strata and a sequence&#13;
stratigraphic frame work for the Paleogene – Neogene section of the Niger Delta.&#13;
This study was therefore designed to establish absolute age using calcareous&#13;
nannofossils for the sediments penetrated by three Wells 1, 2 and 3 in Northwest&#13;
offshore Niger Delta.&#13;
Five hundred and ninety nine ditch cuttings (599) from three wells (1, 2, 3) offshore&#13;
Niger Delta were lithologically examined and lithofacies delineated. Slides from the&#13;
ditch cuttings were prepared using standard procedures and studied using light&#13;
microscopy. The abundance and diversity of the markers of the calcareous&#13;
nannofossils were identified using standard procedures and were used for precise zonal&#13;
delineation and recognition of dated events.&#13;
Greyish to brownish shale, silt and mudstone intercalated with coarse to medium and&#13;
fine-grained sand beds were identified. Forty-one calcareous nannofossil species&#13;
identified confirmed Early Paleocene to Early Pliocene age (NP3-NN15 zones) for the&#13;
three wells. Well 1 penetrated Middle Miocene to Early Pliocene (NN7-NN15 zones);&#13;
Well 2 was restricted to Early to Late Miocene age (NN3-NN11), while Well 3&#13;
encountered the Early Paleocene (NP3-NN4 zones). Established on the first and last&#13;
appearances of the marker species as well as their relative abundances three major&#13;
zones (NN7-NN8, NN9-NN10, NN10 and Younger) four major zones (NN3-NN4,&#13;
NN7, NN8-NN10, NN11) and three major zones (NP3-NP6, NP14-NP21, NN4) were&#13;
identified for well 1, 2 and 3 respectively. The acme events of Discoaster&#13;
prepentaradiatus, Catinaster coalithus, Discoaster kugleri, Helicosphaera&#13;
ampliaperta, Helicosphaera scissura, Pemma basquensis and Chiasmolithus daniscus&#13;
were associated with the 8.80, 9.50, 12.18, 14.20, 15.60, 32.47 and 64.75 Ma&#13;
maximum flooding surfaces, respectively. The correlation of the three wells showed&#13;
basin-ward younging direction and two zones recognized in wells 1 and 2 (NN7 and&#13;
NN8) belonging to the Late Miocene age was confirmed.&#13;
The established zonation scheme for Wells 1, 2 and 3 subdivided the offshore Niger&#13;
Delta Paleocene to Pliocene sequence into zones, subzones and lithostratigraphic&#13;
sequences and hence the absolute age determined
</description>
<pubDate>Sat, 01 Apr 2023 00:00:00 GMT</pubDate>
<guid isPermaLink="false">http://hdl.handle.net/123456789/2139</guid>
<dc:date>2023-04-01T00:00:00Z</dc:date>
</item>
</channel>
</rss>
