ORCID

Abstract

Joint swarms can be important components of fractured reservoirs. They are often explained as damage around faults or related to mechanical differences between layers, although this does not explain the close spacing of the joints. Joint swarms around Bergen (Norway) are described, which are not related to exposed faults and are not influenced by layering or foliation in the Lower Palaeozoic gneisses. We suggest an evolution whereby: (1) a zone of microcracks develops; (2) one microcrack propagates and becomes connected to a source of mineralising fluid; (3) the fracture becomes a microvein, with a higher tensile strength than the microcracked host rock; (4) another microcrack propagates and the cycle is repeated, producing a zone of microveins; (5) the veins are partly weathered out, producing an apparent joint swarm, or the microveins crack at or near the ground-surface. Joint swarms in exposed analogues may therefore not occur at reservoir depths.

DOI

10.1111/ter.12747

Publication Date

2024-08-24

Publication Title

Terra Nova

ISSN

0954-4879

Keywords

fracture corridor, joint swarm, microveins, weathering

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