Hordaland Group

Introduction

The Hordaland Group was originally described by Deegan & Scull (1977) to cover a series of Eocene to Early Miocene marine claystones with minor sandstones (i.e. their Frigg Formation) in the North Sea Tertiary Basin. Subsequently the Hordaland Group has been extended northwards to include the contemporaneous Brygge Formation in the Norwegian Sea (Dalland et al. 1988). In the revised lithostratigraphy of the Norwegian North Sea published by Isaksen & Tonstad (1989) three new sandstones formations were formally assigned to the Hordaland Group, namely the Grid Formation, the Skade Formation and the Vade Formation.

Subsequently, Knox & Holloway (1992) subdivided the terrigenous mudstones of the Hordaland Group in the UK sector into two new separate formations: a lower Horda Formation (Eocene in age) and an upper Lark Formation (Oligocene to Early Miocene in age). The further introduced two new groups to replace the Hordland Group; the lower Stronsay Group (including the Horda Formation and Frigg Sandstone Member) and the upper Westeray Group (including the Larke and Skade formations).

We here suggest to include the use of Horda Formation and the Lark Formation on the Norwegian sector of the North Sea, and to change the status of the sandstone units to members comparable to what has been done in the UK sector. We see, however, no arguments for changing the status of the Hordaland Group and propose to retain this lithostratigraphic unit as originally described by Deegan & Scull (1977).

On Haltenbanken the Hordaland Group consists of claystones and minor sandstones, assigned to the Brygge Formation (Dalland et al., 1988). Presently, no further subdivision exists for the Hordaland Group in the Norwegian Sea. Lateral facies changes and breaks in the sequence may form the basis for future subdivision. The contemporaneous deep-sea (Eocene to mid Miocene) sediments to the west in the Vøring area comprises somewhat different lithologies and may also require a separate lithostratigraphic nomenclature.

Name

English / Norwegian

Hordaland Group / Hordalandgruppen

Derivatio nominis

Named by Deegan & Scull (1977) after the county of Hordaland in Norway.

Original definition

Deegan, C. E. & Scull, B. J. 1977. A standard lithologic nomenclature for the Central and Northern North Sea. Institute of Geological Sciences Report 77/25. NPD Bulletin no. 1, 33 pp.

Lithology

In the North Sea area the Hordaland Group consists of marine claystones with minor sandstones. The claystones are normally light grey to brown, fissile and fossiliferous. Red and green claystones sometimes occur at the base. Thin limestones and streaks of dolomite are present. Sandstones are developed at various levels in the group. These are generally very fine to medium grained, and are often interbed-ded with claystones.

On Haltenbanken the Hordaland Group consists of claystones and minor sandstones, herein assigned to the Brygge Formation. The sandstone content increases to the east.

Thickness

In the North Sea area the group has a thickness of 1060 m in well 2/2-1 and 1365 m in well 24/12-1. Its average thickness is around 1100-1200 m in the central and southern part of the Viking Graben, but in the northern Viking Graben the group only reaches a thickness of a few hundred metres. Maximum thicknesses in the central and southern part of the Viking Graben are approximately 1300 m and 1400 m, respectively. The thickness decreases towards the basin margins.

Geographical distribution

The group is distributed over most of the North Sea Basin. It is incomplete at the basin margins, owing to erosion or non-deposition. The Hordaland Group is also present on the Mid Norwegian Shelf (Dalland et al. 1988), where it occurs throughout Haltenbanken. It thins eastwards and is eroded on the Nordland Ridge.

Boundaries

Lower boundary (basal stratotype)

The lower boundary shows an increase in gamma-ray intensity and a decrease in velocity from the laminated tuffs of the Balder Formation into the claystones of the Hordaland Group. Where the Frigg Member is present at the base of the Hordaland Group the lower boundary normally shows a decrease in gamma-ray response and an increase in velocity from the Balder Formation into the Frigg Member.

Upper boundary (characteristics)

The upper boundary is placed at the contact with undifferentiated grey to grey-brown claystones of the Nordland Group. It represents an unconformity of Middle Miocene age, which may be difficult to identify in some wells.

In the Central Trough, a zone occurs which has high gamma-ray readings and usually a slightly lower velocity than the underlying and overlying claystones. The upper boundary of the Hordaland Group is placed at the base of this zone.

On seismic sections, the sediments below this horizon normally have a distorted signature whilst those above it have a smoother one. The boundary shows a small angular unconformity; it is not clear whether a small hiatus is present. In the Viking Graben, the upper boundary is normally the base of the Utsira Member. The contact is then marked by an upward decrease in gamma-ray intensity (Fig. . ..). Where the basal part of the Nordland Group is developed as claystone the boundary is placed at log breaks associated with a change in claystone colour.

Age

The group is of Eocene to Early Miocene age. Biostratigraphic correlations to wells 2/2-1, 2/2-2 and 2/2-3 indicate that the uppermost part of the Group may be of Middle Miocene age in the Central Trough.

Depositional environment

The Hordaland Group was deposited in an open marine.

Remarks

We here suggest to include the use of the Horda and Lark formations on the Norwegian sector of the North Sea, and to change the status of the sandstone units to members (Grid, Frigg, Vade and Skade members) comparable to what has been done in the UK sector. We see, however, no arguments for changing the status of the Hordaland Group and propose to retain this lithostratigraphic unit as originally described by Deegan & Scull (1977).

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