Skip to main content

Research Repository

Advanced Search

The earthquake cycle in the dry lower continental crust: insights from two deeply exhumed terranes (Musgrave Ranges, Australia and Lofoten, Norway)

Menegon, Luca; Campbell, Lucy; Mancktelow, Neil; Camacho, Alfredo; Wex, Sebastian; Papa, Simone; Toffol, Giovanni; Pennacchioni, Giorgio

Authors

Luca Menegon

Lucy Campbell

Neil Mancktelow

Alfredo Camacho

Sebastian Wex

Simone Papa

Giovanni Toffol

Giorgio Pennacchioni



Abstract

This paper discusses the results of field-based geological investigations of exhumed rocks exposed in the Musgrave Ranges (Central Australia) and in Nusfjord (Lofoten, Norway) that preserve evidence for lower continental crustal earthquakes with focal depths of approximately 25–40 km. These studies have established that deformation of the dry lower continental crust is characterized by a cyclic interplay between viscous creep (mylonitization) and brittle, seismic slip associated with the formation of pseudotachylytes (a solidified melt produced during seismic slip along a fault in silicate rocks). Seismic slip triggers rheological weakening and a transition to viscous creep, which may be already active during the immediate post-seismic deformation along faults initially characterized by frictional melting and wall-rock damage. The cyclical interplay between seismic slip and viscous creep implies transient oscillations in stress and strain rate, which are preserved in the shear zone microstructure. In both localities, the spatial distribution of pseudotachylytes is consistent with a local (deep) source for the transient high stresses required to generate earthquakes in the lower crust. This deep source is the result of localized stress amplification in dry and strong materials generated at the contacts with ductile shear zones, producing multiple generations of pseudotachylyte over geological time. This implies that both the short- and the long-term rheological evolution of the dry lower crust typical of continental interiors is controlled by earthquake cycle deformation.

Citation

Menegon, L., Campbell, L., Mancktelow, N., Camacho, A., Wex, S., Papa, S., …Pennacchioni, G. (2021). The earthquake cycle in the dry lower continental crust: insights from two deeply exhumed terranes (Musgrave Ranges, Australia and Lofoten, Norway). Philosophical transactions. Series A, Mathematical, physical, and engineering sciences, 379(2193), Article 20190416. https://doi.org/10.1098/rsta.2019.0416

Journal Article Type Article
Acceptance Date Sep 14, 2020
Online Publication Date Feb 1, 2021
Publication Date Mar 22, 2021
Deposit Date Apr 3, 2022
Publicly Available Date Mar 29, 2024
Journal Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences
Print ISSN 1364-503X
Electronic ISSN 1471-2962
Publisher The Royal Society
Peer Reviewed Peer Reviewed
Volume 379
Issue 2193
Article Number 20190416
DOI https://doi.org/10.1098/rsta.2019.0416
Keywords Lower crustal earthquakes; Pseudotachylytes; Ductile shear zones; Transient deformation; Dry lower continental crust
Public URL https://hull-repository.worktribe.com/output/3752778

Files





You might also like



Downloadable Citations