The Flora Field, Blocks 31/26a, 31/26c, UK North Sea

Author:

Hayward R. D.1,Martin C. A. L.1,Harrison D.1,Van Dort G.1,Guthrie S.1,Padget N.1

Affiliation:

1. Amerada Hess E&P33 Grosvenor Place, London SW1X 7HY, UK

Abstract

AbstractThe Flora Field straddles Blocks 31/26a and 31/26c of the UK sector of the North Sea on the southern margin of the Central Graben. The field is located on the Grensen Nose, a long-lived structural high, and was discovered by the Amerada Hess operated well 31/26a-12 in mid-1997.The Flora Field accumulation is reservoired within the Flora Sandstone, an Upper Carboniferous fluvial deposit, and a thin Upper Jurassic veneer, trapped within a tilted fault block. Oil is sourced principally from the Kimmeridge Clay Formation of the Central Graben and is sealed by overlying Lower Cretaceous marls and Upper Cretaceous Chalk Group.Reservoir quality is generally good with average net/gross of 85% and porosity of 21%, although permeability (Kh) exhibits a great deal of heterogeneity with a range of 0.1 to <10000mD (average 300 mD). The reservoir suffers both sub-horizontal (floodplain shales) and vertical (faults) compartmentalization, as well as fracturing and a tar mat at the oil-water contact modifying flow and sweep of the reservoir. Expected recoverable reserves currently stand at 13 MMBBL

Publisher

Geological Society of London

Subject

Geology

Reference11 articles.

1. Cameron T. D. J. (1993a) Lithostratigraphic nomenclature of the UK North Sea Volume 4. Triassic, Permian and Pre-Permian (Central and Northern North Sea), eds Knox R. W. O'B Cordey W. G.

2. Cameron T. D. J. (1993b) Lithostratigraphic nomenclature of the UK North Sea Volume 5. Carboniferous of the Southern North Sea, eds Knox R. W. O'B Cordey W. G.

3. Chadwick R. A. Holliday D. W. Holloway S. Hulbert A. G. (1995) The structure and evolution of the Northumberland-Solway Basin and adjacent areas, British Geological Survey Subsurface Memoir.

4. Dixon J. E. Fitton J. G. Frost R. T. C. (1981) in Petroleum Geology of the Continental Shelf of Northwest Europe, The Tectonic significance of Post-Carboniferous ligneous activity in the North Sea Basin, eds Illing L. V. Hobson G. D. (Heyden & Son, London), pp 121–137.

5. Folk R. L. (1980) Petrology of sedimentary rocks (Austin, Hemphill).

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