The Cenomanian to Maastrictian foraminifera have been studied from
borehole material (ditchcuttings) of three wells - 44/2-1,49/19-1 and
49/20-2 - drilled by Shell (UK) Exploration & Production Ltd in the
Southern North Sea Basin. The microfaunas have been utilized in the
formulation of a zonal scheme comprising twelve foraminiferal biozones
based on 'tops' (highest occurrences) of selected taxa; the taxonomy of
the stratigraphically diagnostic forms is briefly discussed.
The major lithostratigraphic units of the Dutch and British sectors
of the Upper Cretaceous of the Southern North Sea Basin are recognised
from Gamma Ray and Formation Density wireline log signitures (where
available); these are the Chalk Group and the Texel and Ommelanden
Formations.
. The biozones are related to the lithostratigraphic units in the
three well sections and these are correlated across the Southern North
Sea Basin. The dating and correlation of the sequences shows
significant differences in thicknesses to exist between the sections;
these are tentatively related to position relative to 'palaeo-highs',
differential subsidence and/or uplift along inversion axes in the area.
Date of Award | 1985 |
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Original language | English |
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Awarding Institution | |
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Sponsors | NERC and Shell (UK) Exploration & Production Ltd. |
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A Foraminiferal Biostratigraphy of the Upper Cretaceous of the Southern North Sea Basin (UK Sector).
Ball, K. C. (Author). 1985
Student thesis: PhD