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The AAPG/Datapages Combined Publications Database

AAPG Bulletin


AAPG Bulletin, V. 89, No. 3 (March 2005), P. 383-401.

Copyright copy2005. The American Association of Petroleum Geologists. All rights reserved.

Pressure solution in chalk

M. Safaricz,1 I. Davison2

1Department of Geology, Royal Holloway, University of London, Egham, Surrey TW20 0EX, United Kingdom; present address: Universitaumlt Potsdam, Institut fuumlr Geowissenschaften, Postfach 60 15 53, 14415 Potsdam, Germany; [email protected]
2Earthmoves Ltd., Chartley House, 38-42 Upper Park Road, Camberley, Surrey, GU15 2EF, United Kingdom; [email protected]


Pressure-solution residues in the Cretaceous to Paleocene chalk from the North Sea area were studied to understand the pressure-solution process and fluid flow. Residue seams reach lengths and thickness of more than 800 and 0.15 m (2625 and 0.5 ft), respectively. Seams can present significant barriers to fluid flow because they have nannodarcy permeability and hold back large pressure differentials.

Stylolite amplitudes decrease when they merge, making it difficult to quantify volume loss. Measuring amplitudes allows volume-loss estimates using a new dissolution ratio method. The sum of the thicknesses of all residues is multiplied by the maximum amplitude-to-residue thickness ratio. On average, 30 mm (1.2 in.) of chalk had to be dissolved to produce a 1-mm (0.04-in.)-thick residue. The volume loss of chalk from Flamborough averages about 50% and is 60% in the Machar oil field, United Kingdom Central Graben.

The minimum fluid volume required to produce the volume loss in 1 unit volume of preserved chalk on the Machar field is estimated to be 8000 unit volumes. This and the stable isotopes of vein carbonates imply that the pressure-solution process involved an open-fluid system. High illite content in mixed layered illite-smectite and high illite crystallinity of clays in the pressure-solution seams in the Machar reservoir indicate high diagenetic maturity, with implied temperatures in the range of 200–360degC (392–680degF), which is greater than the present-day reservoir temperature of 85degC (185degF). The anomalously hot temperatures are interpreted to be produced by deep mineralizing fluids transported from the Central Graben. The lack of abundant veining in the chalk and the large fluid volumes involved in the chalk dissolution suggest that this was an open pressure-solution system.

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