Journal of Petroleum Geology, Vol.7,
No.2, pp.169-188, 1984
©Copyright 2000 Scientific Press,
Ltd.
SEDIMENTOLOGICAL AND
PALEONTOLOGICAL ANALYSES OF
JURASSIC NORTH SEA DEPOSITS FROM DELTAIC ENVIRONMENTS
J. Nagy*, H. Dypvik* and T.
Bjaerke*
*Institutt for Geologi,
Universitetet 1 Oslo, Postboks 1047, Blindern, Oslo 3, Norway.
Abstract
Core samples from Well 33/9-3, Norwegian
North Sea, have been analysed sedimentologically, palynologically
and micro-paleontologically. The cores cover the Toarcian Drake
Member of the Dunlin Formation, and nearly the whole thickness of
the Middle Jurassic Brent Formation. The Drake Member is
characterized by pro-deltaic depositional conditions. In the
Brent Formation, five members are recognized (from below): the
Broom, Rannoch and Etive Members represent distributary mouth bar
facies; while the Ness and Tarbert Members are recognized as
interdistributary bay fill sequences. The composition of the
kerogen assemblages is controlled by the changing energy regimes
of the different depositional facies. Terrestrial plant débris
are dominant throughout the studied interval. Marine palynomorphs
are present in the Drake Member and in the lower part of the
Broom Member. The development of rich, arenaceous foraminiferal
assemblages in the Drake Member are interpreted as a response to
shallow, pro-deltaic conditions. Calcareous foraminifera
constitute only a small, accessorial part of these assemblages.