Item talk:Q151362
From geokb
DOI:
DOI: 10.1002/2016jb013124 ISSN: - 2169-9313 - 2169-9356 URL: http://dx.doi.org/10.1002/2016JB013124 abstract: "<jats:title>Abstract</jats:title><jats:p>Great subduction earthquakes\ \ are thought to rupture portions of the megathrust, where interseismic coupling\ \ is high and velocity\u2010weakening frictional behavior is dominant, releasing\ \ elastic deformation accrued over a seismic cycle. Conversely, postseismic afterslip\ \ is assumed to occur primarily in regions of velocity\u2010strengthening frictional\ \ characteristics that may correlate with lower interseismic coupling. However,\ \ it remains unclear if fixed frictional properties of the subduction interface,\ \ coseismic or aftershock\u2010induced stress redistribution, or other factors\ \ control the spatial distribution of afterslip. Here we use interferometric synthetic\ \ aperture radar and Global Position System observations to map the distribution\ \ of coseismic slip of the 2015 <jats:italic>M<jats:sub>w</jats:sub></jats:italic>\ \ 8.3 Illapel, Chile, earthquake and afterslip within the first 38\u2009days following\ \ the earthquake. We find that afterslip overlaps the coseismic slip area and\ \ propagates along\u2010strike into regions of both high and moderate interseismic\ \ coupling. The significance of these observations, however, is tempered by the\ \ limited resolution of geodetic inversions for both slip and coupling. Additional\ \ afterslip imaged deeper on the fault surface bounds a discrete region of deep\ \ coseismic slip, and both contribute to net uplift of the Chilean Coastal Cordillera.\ \ A simple partitioning of the subduction interface into regions of fixed frictional\ \ properties cannot reconcile our geodetic observations. Instead, stress heterogeneities,\ \ either preexisting or induced by the earthquake, likely provide the primary\ \ control on the afterslip distribution for this subduction zone earthquake. We\ \ also explore the occurrence of coseismic and postseismic coastal uplift in this\ \ sequence and its implications for recent hypotheses concerning the source of\ \ permanent coastal uplift along subduction zones.</jats:p>" alternative-id: - 10.1002/2016JB013124 author: - affiliation: - name: Department of Earth and Environmental Sciences University of Iowa Iowa City Iowa USA family: Barnhart given: William D. sequence: first - affiliation: - name: Earthquake Science Center U.S. Geological Survey Menlo Park California USA family: Murray given: Jessica R. sequence: additional - affiliation: - name: Geological Hazards Science Center U.S. Geological Survey Golden Colorado USA family: Briggs given: Richard W. sequence: additional - affiliation: - name: Department of Geological Sciences University of Missouri Columbia Missouri USA family: Gomez given: Francisco sequence: additional - affiliation: - name: Department of Geological Sciences University of Missouri Columbia Missouri USA family: Miles given: Charles P. 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'@context': https://schema.org '@type': CreativeWork about: - '@type': Place additionalType: country identifier: '@type': PropertyValue propertyID: GeoKB value: https://geokb.wikibase.cloud/entity/Q31 name: Chile abstract: "Great subduction earthquakes are thought to rupture portions of the megathrust,\ \ where interseismic coupling is high and velocity-weakening frictional behavior\ \ is dominant, releasing elastic deformation accrued over a seismic cycle. Conversely,\ \ postseismic afterslip is assumed to occur primarily in regions of velocity-strengthening\ \ frictional characteristics that may correlate with lower interseismic coupling.\ \ However, it remains unclear if fixed frictional properties of the subduction\ \ interface, coseismic or aftershock-induced stress redistribution, or other factors\ \ control the spatial distribution of afterslip. Here we use interferometric synthetic\ \ aperture radar and Global Position System observations to map the distribution\ \ of coseismic slip of the 2015 Mw 8.3 Illapel, Chile, earthquake and afterslip\ \ within the first 38\u2009days following the earthquake. We find that afterslip\ \ overlaps the coseismic slip area and propagates along-strike into regions of\ \ both high and moderate interseismic coupling. The significance of these observations,\ \ however, is tempered by the limited resolution of geodetic inversions for both\ \ slip and coupling. Additional afterslip imaged deeper on the fault surface bounds\ \ a discrete region of deep coseismic slip, and both contribute to net uplift\ \ of the Chilean Coastal Cordillera. A simple partitioning of the subduction interface\ \ into regions of fixed frictional properties cannot reconcile our geodetic observations.\ \ Instead, stress heterogeneities, either preexisting or induced by the earthquake,\ \ likely provide the primary control on the afterslip distribution for this subduction\ \ zone earthquake. We also explore the occurrence of coseismic and postseismic\ \ coastal uplift in this sequence and its implications for recent hypotheses concerning\ \ the source of permanent coastal uplift along subduction zones." additionalType: Article author: - '@type': Person affiliation: - '@type': Organization identifier: '@type': PropertyValue propertyID: GeoKB value: https://geokb.wikibase.cloud/entity/Q44231 name: Geologic Hazards Science Center email: wbarnhart@usgs.gov familyName: Barnhart givenName: William D. identifier: - '@type': PropertyValue propertyID: GeoKB value: https://geokb.wikibase.cloud/entity/Q44667 name: Barnhart, William D. wbarnhart@usgs.gov position: 1 - '@type': Person affiliation: - '@type': Organization identifier: '@type': PropertyValue propertyID: GeoKB value: https://geokb.wikibase.cloud/entity/Q44278 name: Earthquake Science Center email: jrmurray@usgs.gov familyName: Murray givenName: Jessica R. identifier: - '@type': PropertyValue propertyID: ORCiD value: 0000-0002-6144-1681 - '@type': PropertyValue propertyID: GeoKB value: https://geokb.wikibase.cloud/entity/Q48219 name: Murray, Jessica R. jrmurray@usgs.gov position: 2 - '@type': Person affiliation: - '@type': Organization identifier: '@type': PropertyValue propertyID: GeoKB value: https://geokb.wikibase.cloud/entity/Q44231 name: Geologic Hazards Science Center email: rbriggs@usgs.gov familyName: Briggs givenName: Richard W. identifier: - '@type': PropertyValue propertyID: ORCiD value: 0000-0001-8108-0046 - '@type': PropertyValue propertyID: GeoKB value: https://geokb.wikibase.cloud/entity/Q45002 name: Briggs, Richard W. rbriggs@usgs.gov position: 3 - '@type': Person affiliation: [] familyName: Gomez givenName: Francisco identifier: [] name: Gomez, Francisco position: 4 - '@type': Person affiliation: [] familyName: Miles givenName: Charles P. J. identifier: [] name: Miles, Charles P. J. position: 5 - '@type': Person affiliation: - '@type': Organization identifier: '@type': PropertyValue propertyID: GeoKB value: https://geokb.wikibase.cloud/entity/Q44278 name: Earthquake Science Center email: jsvarc@usgs.gov familyName: Svarc givenName: Jerry L. identifier: - '@type': PropertyValue propertyID: ORCiD value: 0000-0002-2802-4528 - '@type': PropertyValue propertyID: GeoKB value: https://geokb.wikibase.cloud/entity/Q54099 name: Svarc, Jerry L. jsvarc@usgs.gov position: 6 - '@type': Person affiliation: [] familyName: Riquelme givenName: "Seb\xE1stian" identifier: [] name: "Riquelme, Seb\xE1stian" position: 7 - '@type': Person affiliation: [] familyName: Stressler givenName: Bryan J. identifier: [] name: Stressler, Bryan J. position: 8 dateModified: '2017-03-13T13:54:13' datePublished: '2016' funder: - '@type': Organization identifier: '@type': PropertyValue propertyID: GeoKB value: https://geokb.wikibase.cloud/entity/Q44278 name: Earthquake Science Center url: https://www.usgs.gov/centers/earthquake-science-center identifier: - '@type': PropertyValue propertyID: GeoKB value: https://geokb.wikibase.cloud/entity/Q151362 - '@type': PropertyValue propertyID: USGS PW IndexID value: 70184989 - '@type': PropertyValue propertyID: DOI value: 10.1002/2016JB013124 name: 'Coseismic slip and early afterslip of the 2015 Illapel, Chile, earthquake: Implications for frictional heterogeneity and coastal uplift' publisher: '@type': Organization name: AGU Publications
