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AAPG Bulletin

Abstract

AAPG Bulletin, V. 93, No. 7 (July 2009), P. 919-938.

Copyright copy2009. The American Association of Petroleum Geologists. All rights reserved.

DOI:10.1306/03270908161

Spatial variation of microstructure and petrophysical properties along deformation bands in reservoir sandstones

Anita Torabi,1 Haakon Fossen2

1Centre for Integrated Petroleum Research, Unifob Petroleum, University of Bergen, Post Box 7800, 5020 Bergen, Norway; [email protected]
2Centre for Integrated Petroleum Research/Department of Earth Science, University of Bergen, Post Box 7800, 5020 Bergen, Norway; [email protected]

ABSTRACT

A series of deformation bands Previous HitfromNext Hit various reservoir sandstones deformed at different burial depths have been studied with respect to microstructural and petrophysical variations. In many of the examples explored, the internal microstructure, porosity, and Previous HitpermeabilityNext Hit vary along the bands at the centimeter or even millimeter scale, changing and in most cases reducing the ability of the bands to act as barriers to fluid flow. Porosity varies by up to 18% and Previous HitpermeabilityNext Hit by up to two orders of magnitude. Such petrophysical variations are found along different types of deformation bands, but the range depends upon the deformation mechanisms, in particular on the degree of cataclasis and dissolution in cataclastic and dissolution bands, and on the phyllosilicate content in disaggregation bands. For cataclastic bands, the grain-size distribution changes along the bands with regard to the degree of cataclasis. Furthermore, the increased specific surface area of the pore-grain interface as a result of cataclasis causes higher Previous HitpermeabilityNext Hit reduction in cataclastic bands than in other types of deformation bands. Phyllosilicate content can influence the thickness of phyllosilicate bands. However, no apparent correlation between thickness and intensity of cataclasis in the studied cataclastic deformation bands is observed.

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