| There, fault planes parallel to the fjord display red coloration, red cataclasite in zones up to 10 cm thick, and wide zones of unconsolidated breccia or gouge. |
| The margins are straight, with discordant injection veins, and grade into a marginal cataclasite zone adjacent to the mylonite. |
| Type I corresponds to the less deformed limestone, which contains cataclasite bands, veins and, at times, preserved sedimentary fabrics. |
