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dc.contributor.authorMenegon, Len
dc.contributor.authorCampbell, Len
dc.contributor.authorMancktelow, Nen
dc.contributor.authorCamacho, Aen
dc.contributor.authorWex, Sen
dc.contributor.authorPapa, Sen
dc.contributor.authorToffol, Gen
dc.contributor.authorPennacchioni, Gen
dc.date.accessioned2021-10-13T12:17:53Z
dc.date.available2021-10-13T12:17:53Z
dc.date.issued2021-03-22en
dc.identifier.issn1364-503Xen
dc.identifier.other20190416en
dc.identifier.urihttp://hdl.handle.net/10026.1/18046
dc.description.abstract

<jats:p>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.</jats:p> <jats:p>This article is part of a discussion meeting issue ‘Understanding earthquakes using the geological record’.</jats:p>

en
dc.languageenen
dc.language.isoenen
dc.publisherRoyal Society, Theen
dc.titleThe earthquake cycle in the dry lower continental crust: insights from two deeply exhumed terranes (Musgrave Ranges, Australia and Lofoten, Norway)en
dc.typeJournal Article
plymouth.issue2193en
plymouth.volume379en
plymouth.journalPhilosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciencesen
dc.identifier.doi10.1098/rsta.2019.0416en
plymouth.organisational-group/Plymouth
plymouth.organisational-group/Plymouth/Faculty of Science and Engineering
plymouth.organisational-group/Plymouth/Faculty of Science and Engineering/School of Geography, Earth and Environmental Sciences
plymouth.organisational-group/Plymouth/REF 2021 Researchers by UoA
plymouth.organisational-group/Plymouth/REF 2021 Researchers by UoA/UoA07 Earth Systems and Environmental Sciences
dcterms.dateAccepted2020-09-14en
dc.rights.embargodate2021-10-14en
dc.identifier.eissn1471-2962en
dc.rights.embargoperiodNot knownen
rioxxterms.versionofrecord10.1098/rsta.2019.0416en
rioxxterms.licenseref.urihttp://www.rioxx.net/licenses/all-rights-reserveden
rioxxterms.licenseref.startdate2021-03-22en
rioxxterms.typeJournal Article/Reviewen


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