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dc.contributor.authorLiu, Shaozhuo
dc.contributor.authorXu, Xiwei
dc.contributor.authorKlinger, Yann
dc.contributor.authorNocquet, Jean-Mathieu
dc.contributor.authorChen, Guihua
dc.contributor.authorYu, Guihua
dc.contributor.authorJonsson, Sigurjon
dc.date.accessioned2019-11-11T14:50:17Z
dc.date.available2019-11-11T14:50:17Z
dc.date.issued2019-11-06
dc.identifier.citationLiu, S., Xu, X., Klinger, Y., Nocquet, J., Chen, G., Yu, G., & Jónsson, S. (2019). Lower crustal heterogeneity beneath the northern Tibetan Plateau constrained by GPS measurements following the 2001 Mw7.8 Kokoxili earthquake. Journal of Geophysical Research: Solid Earth. doi:10.1029/2019jb017732
dc.identifier.doi10.1029/2019jb017732
dc.identifier.urihttp://hdl.handle.net/10754/659978
dc.description.abstractWe use Global Positioning System (GPS) measurements across the Xidatan segment of the Kunlun fault in the Tibetan Plateau to investigate the surface deformation following the 2001 Mw 7.8 Kokoxili earthquake. We find significant post-seismic deformation during the period 2007-2015, characterized by an asymmetric shear across the 2001 rupture, with average velocities reaching ~10 mm/yr about 30-45 km south of the coseismic rupture. We also find that the postseismic transients diffused away from the coseismic rupture through time, with a shift of the maximum transient rates from ~20-30 km south of the rupture in 2001-2002 to ~30-45 km in 2007-2015. Viscoelastic relaxation is the dominant physical process during the period 2007-2015. The estimated effective viscosity of the lower crust beneath the Songpan-Ganzi terrane is 2×1018-3×1018 Pa s from the 2001-2002 data, and it has increased to ~2×1019 Pa s for the period 6 to 14 years after the event. The large asymmetry in the postseismic deformation field indicates a laterally heterogeneous lower crust beneath the northern Tibetan Plateau. Viscoelastic relaxation models show that the viscosity of the lower crust beneath the Qaidam basin is ~2 and ~4 times larger than the viscosity of the lower crust beneath the Songpan-Ganzi terrane in 2001-2002 and 2007-2015, respectively. Based on these data and results from previous studies, we postulate that the Kunlun fault itself is not the unique rheological boundary and that additional domains with viscosity increasing from the Qiangtang terrane to the Qaidam basin appear to be required.
dc.publisherAmerican Geophysical Union (AGU)
dc.relation.urlhttps://onlinelibrary.wiley.com/doi/abs/10.1029/2019JB017732
dc.rightsArchived with thanks to Journal of Geophysical Research: Solid Earth
dc.subjectNorthern Tibetan Plateau
dc.subjectKunlun fault
dc.subject2001 Mw7.8 Kokoxili earthquake
dc.subjectpostseismic deformation
dc.subjectGPS
dc.subjectlower crustal heterogeneity
dc.titleLower crustal heterogeneity beneath the northern Tibetan Plateau constrained by GPS measurements following the 2001 Mw7.8 Kokoxili earthquake
dc.typeArticle
dc.contributor.departmentCrustal Deformation and InSAR Group
dc.contributor.departmentEarth Science and Engineering Program
dc.contributor.departmentPhysical Science and Engineering (PSE) Division
dc.identifier.journalJournal of Geophysical Research: Solid Earth
dc.eprint.versionPost-print
dc.contributor.institutionKey Laboratory of Active Tectonics and Volcano, Institute of Geology, China Earthquake Administration Beijing China
dc.contributor.institutionUniversité de Paris, Institut de physique du globe de Paris, CNRS Paris France
dc.contributor.institutionInstitute of Crustal Dynamics, China Earthquake Administration Beijing China
dc.contributor.institutionGeoazur, IRD, Université Côte d'Azur, CNRS, Observatoire de la Côte d'Azur Valbonne France
kaust.personLiu, Shaozhuo
kaust.personJonsson, Sigurjon
refterms.dateFOA2019-11-11T14:52:32Z


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