Fig. 1 Structure of the lower crustal fault in the Bergen Arcs.

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Fig. 1 Structure of the lower crustal fault in the Bergen Arcs. Structure of the lower crustal fault in the Bergen Arcs. (A) The damage zone is present on the northern side of the fault and is locally intruded by injection veins branching from the pseudotachylyte (Pst). (B) The interior of the fault consists of a zoned pseudotachylyte (inner and outer pseudotachylyte) bounded by cataclasites. The wall rock contains garnet (Grt), plagioclase (Plg), and diopside (Di). Clasts of cataclasite have been entrained in the outer pseudotachylyte (white arrows). (C) The damage zone contains fragmented wall rock minerals with little to no shear strain. Along this portion of the fault, cataclasites are absent. North is up in (B) and (C). (D) X-ray computed microtomography image of the fault shown in (B). The outer pseudotachylyte and wall rock plagioclase are transparent for better three-dimensional rendering. The orientation of the reference frame is as follows: x, west; y, perpendicular to the topographic surface; and z, north. Photo credit: (A, B, and C) Arianne Petley-Ragan, University of Oslo and (D) Francois Renard, University of Oslo. Arianne Petley-Ragan et al. Sci Adv 2019;5:eaaw0913 Copyright © 2019 The Authors, some rights reserved; exclusive licensee American Association for the Advancement of Science. No claim to original U.S. Government Works. Distributed under a Creative Commons Attribution NonCommercial License 4.0 (CC BY-NC).