Searle, M, Avouac, J-P, Elliott, J orcid.org/0000-0003-2957-4596 et al. (1 more author) (2017) Ductile shearing to brittle thrusting along the Nepal Himalaya: Linking Miocene channel flow and critical wedge tectonics to 25th April 2015 Gorkha earthquake. Tectonophysics, 714-71. pp. 117-124. ISSN 0040-1951
Abstract
The 25th April 2015 magnitude 7.8 Gorkha earthquake in Nepal ruptured the Main Himalayan thrust (MHT) for ~ 140 km east-west and ~ 50 km across strike. The earthquake nucleated at a depth of ~ 15–18 km approximating to the brittle-ductile transition and propagated east along the MHT but did not rupture to the surface, leaving half of the fault extent still locked beneath the Siwalik hills. Coseismic slip shows that motion is confined to the ramp-flat geometry of the MHT and there was no out-of-sequence movement along the Main Central Thrust (MCT). Below 20 km depth, the MHT is a creeping, aseismic ductile shear zone. Cumulated deformation over geological time has exhumed the deeper part of the Himalayan orogen which is now exposed in the Greater Himalaya revealing a tectonic history quite different from presently active tectonics. There, early Miocene structures, including the MCT, are almost entirely ductile, with deformation occurring at temperatures higher than ~ 400 °C, and were active between ~ 22–16 Ma. Kyanite and sillimanite-grade gneisses and migmatites approximately 5–20 km thick in the core of the Greater Himalayan Sequence (GHS) together with leucogranite intrusions along the top of the GHS were extruded southward between ~ 22–15 Ma, concomitant with ages of partial melting. Thermobarometric constraints show that ductile extrusion of the GHS during the Miocene occurred at muscovite-dehydration temperatures ~ 650-775 °C, and thus brittle thrusting and critical taper models for GHS deformation are unrealistic. As partial melting and channel flow ceased at ~ 15 Ma, brittle thrusting and underplating associated with duplex formation occurred along the Lesser Himalaya passively uplifting the GHS.
Metadata
Item Type: | Article |
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Authors/Creators: |
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Copyright, Publisher and Additional Information: | © 2016 Published by Elsevier B.V. This is an author produced version of a paper published in Tectonophysics. Uploaded in accordance with the publisher's self-archiving policy. |
Keywords: | Gorkha earthquake; Nepal; Himalaya; Channel flow; Critical wedge |
Dates: |
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Institution: | The University of Leeds |
Academic Units: | The University of Leeds > Faculty of Environment (Leeds) > School of Earth and Environment (Leeds) > Inst of Geophysics and Tectonics (IGT) (Leeds) |
Depositing User: | Symplectic Publications |
Date Deposited: | 17 Oct 2016 10:44 |
Last Modified: | 03 Jan 2018 15:02 |
Published Version: | http://dx.doi.org/10.1016/j.tecto.2016.08.003 |
Status: | Published |
Publisher: | Elsevier |
Identification Number: | 10.1016/j.tecto.2016.08.003 |
Open Archives Initiative ID (OAI ID): | oai:eprints.whiterose.ac.uk:106049 |