Geodetic imaging of late postseismic lower crustal flow in Tibet

Ryder, Isabelle, Wang, Hua, Bie, Lidong and Rietbrock, Andreas (2014) Geodetic imaging of late postseismic lower crustal flow in Tibet. Earth and Planetary Science Letters, 404. pp. 136-143. ISSN 0012-821X

Full text not available from this repository.

Abstract

Integral to understanding past and present seismotectonic activity in orogenic zones is whether any part of the lower crust is weak enough to flow, since a weak zone at depth influences the style of deformation that occurs. Thick crust such as found beneath the Tibetan Plateau and the Altiplano-Puna Plateau in the Andes leads to elevated temperatures at depth, which potentially allows the lower crust to flow on human time scales, as well as on the time scales of plateau formation and evolution. Here we use the late postseismic response of the crust to large earthquakes as a tool for investigating rheological structure beneath the Tibetan Plateau. Eighteen years (1992-2010) of InSAR data on the southern Tibetan Plateau show a late postseismic relaxation response to two large earthquakes in 1951 and 1952. The relaxation occurs throughout a thick viscoelastic lower crust and possibly extends into the upper mantle. The lower crust has viscosity 6-10 × 1019 Pas, with an associated Maxwell relaxation time of 63 years. Flow within a thin mid-crustal channel can be ruled out. These late-stage postseismic observations represent the first clear evidence of present-day lower crustal flow, and are consistent with geophysical evidence for fluid-weakened lower crust across much of the Tibetan Plateau, as required by models of plateau formation. Active deformation of continental plateaus in other parts of the world, notably the Altiplano-Puna Plateau in South America, may also be strongly influenced by a weak lower crust.

Item Type: Article
Additional Information: Funding Information: ERS and Envisat data were obtained from the European Space Agency through a Dragon-3 project ( 10607 ). H.W. was supported by the NSFC ( 41104016 ) and the State Key Laboratory of Earth Dynamics ( LED2013B04 ). We thank Roland Burgmann for making valuable comments on an early draft of this manuscript.
Uncontrolled Keywords: beng co,insar,lower crustal flow,postseismic,tibetan plateau,geophysics,geochemistry and petrology,earth and planetary sciences (miscellaneous),space and planetary science ,/dk/atira/pure/subjectarea/asjc/1900/1908
Related URLs:
Depositing User: LivePure Connector
Date Deposited: 22 Apr 2022 10:30
Last Modified: 08 Jun 2022 14:46
URI: https://ueaeprints.uea.ac.uk/id/eprint/84739
DOI: 10.1016/j.epsl.2014.07.026

Actions (login required)

View Item View Item