A recent deep earthquake doublet in light of long-term evolution of Nazca subduction
| dc.contributor.author | Zahradnik, Jindrich | |
| dc.contributor.author | Čížková, Hana | |
| dc.contributor.author | Bina, Craig R. | |
| dc.contributor.author | Sokos, Efthimios N. | |
| dc.contributor.author | Jánský, Jirí | |
| dc.contributor.author | Tavera, Hernando | |
| dc.contributor.author | Carvalho, João | |
| dc.date.accessioned | 2018-08-03T14:40:58Z | |
| dc.date.available | 2018-08-03T14:40:58Z | |
| dc.date.issued | 2017-03-31 | |
| dc.description.abstract | Earthquake faulting at ~600 km depth remains puzzling. Here we present a new kinematic interpretation of two Mw7.6 earthquakes of November 24, 2015. In contrast to teleseismic analysis of this doublet, we use regional seismic data providing robust two-point source models, further validated by regional back-projection and rupture-stop analysis. The doublet represents segmented rupture of a ∼30-year gap in a narrow, deep fault zone, fully consistent with the stress field derived from neighbouring 1976-2015 earthquakes. Seismic observations are interpreted using a geodynamic model of regional subduction, incorporating realistic rheology and major phase transitions, yielding a model slab that is nearly vertical in the deep-earthquake zone but stagnant below 660 km, consistent with tomographic imaging. Geodynamically modelled stresses match the seismically inferred stress field, where the steeply down-dip orientation of compressive stress axes at ∼600 km arises from combined viscous and buoyant forces resisting slab penetration into the lower mantle and deformation associated with slab buckling and stagnation. Observed fault-rupture geometry, demonstrated likelihood of seismic triggering, and high model temperatures in young subducted lithosphere, together favour nanometric crystallisation (and associated grain-boundary sliding) attending high-pressure dehydration as a likely seismogenic mechanism, unless a segment of much older lithosphere is present at depth. | es_ES |
| dc.description.peer-review | Por pares | es_ES |
| dc.format | application/pdf | es_ES |
| dc.identifier.citation | Zahradnik, J., Čížková, H., Bina, C. R., Sokos, E., Jánský, J., Tavera, H., & Carvalho, J. (2017). A recent deep earthquake doublet in light of long-term evolution of Nazca subduction.==$Scientific Reports, 7,$==45153. https://doi.org/10.1038/srep45153 | es_ES |
| dc.identifier.doi | https://doi.org/10.1038/srep45153 | es_ES |
| dc.identifier.govdoc | index-oti2018 | |
| dc.identifier.journal | Scientific Reports | es_ES |
| dc.identifier.uri | http://hdl.handle.net/20.500.12816/2224 | |
| dc.language.iso | eng | es_ES |
| dc.publisher | Nature Research | es_ES |
| dc.relation.ispartof | urn:issn:2045-2322 | |
| dc.rights | info:eu-repo/semantics/closedAccess | es_ES |
| dc.subject | Geodynamics | es_ES |
| dc.subject | Seismology | es_ES |
| dc.subject | Subduction | es_ES |
| dc.subject.ocde | http://purl.org/pe-repo/ocde/ford#1.05.00 | es_ES |
| dc.subject.ocde | http://purl.org/pe-repo/ocde/ford#1.05.04 | es_ES |
| dc.title | A recent deep earthquake doublet in light of long-term evolution of Nazca subduction | es_ES |
| dc.type | info:eu-repo/semantics/article | es_ES |