The crustal structure of the western Himalayas and Tibet

Gilligan, Amy and Priestley, Keith F. and Roecker, Steven W. and Levin, Vadim and Rai, S. S. (2015) The crustal structure of the western Himalayas and Tibet. Journal of Geophysical Research: Solid Earth, 120 (5). pp. 3946-3964. ISSN 2156-2202 DOI https://doi.org/10.1002/2015JB011891

[img]
Preview
Text
jgrb51145.pdf - Published Version

Download (5MB) | Preview
[img]
Preview
Image
image_n_jgrb51145-fig-0001.png - Published Version

Download (438kB) | Preview
[img] Text
jgrb51145-sup-0001-gilliganetalsupinfo.doc - Supplemental Material

Download (90kB)
[img] Text
jgrb51145-sup-0002-WTmohodepths.csv - Supplemental Material

Download (3kB)
Official URL: http://dx.doi.org/10.1002/2015JB011891

Abstract

We present new, high-resolution, shear velocity models for the western Himalayas and West Tibet from the joint inversion of P receiver functions recorded using seismic stations from four arrays in this region and fundamental mode Rayleigh wave group velocity maps from 5–70 s covering Central and Southern Asia. The Tibetan Plateau is a key locality in understanding large-scale continental dynamics. A large number of investigations has examined the structure and processes in eastern Tibet; however, western Tibet remains relatively understudied. Previous studies in this region indicate that the western part of the Tibetan Plateau is not a simple extension of the eastern part. The areas covered by these arrays include the Karakoram and Altan-Tagh faults, and major terrane boundaries in West Tibet and the Himalayas. The arrays used include broadband data collected by the West Tibet Array, a U.S.-China deployment on the western side of the Tibetan Plateau between 2007 and 2011. We use the shear wave velocity models to obtain estimates of Moho depth. The Moho is deep (68–84 km) throughout West Tibet. We do not observe significant steps within the Moho beneath West Tibet. A large step in Moho depth is observed at the Altyn-Tagh fault, where Moho depths are 20–30 km shallower to the north of the fault compared to those to the south. Beneath the Lhasa Terrane and Tethyan Himalayas, we observe a low-velocity zone in the midcrust. This feature is not interrupted by the Karakoram Fault, suggesting that the Karakoram Fault does not cut through the entire crust.

Item Type: Article
Uncontrolled Keywords: 2015AREP; IA69;
Subjects: 02 - Geodynamics, Geophysics and Tectonics
Divisions: 02 - Geodynamics, Geophysics and Tectonics
08 - Green Open Access
Journal or Publication Title: Journal of Geophysical Research: Solid Earth
Volume: 120
Page Range: pp. 3946-3964
Identification Number: https://doi.org/10.1002/2015JB011891
Depositing User: Sarah Humbert
Date Deposited: 25 Aug 2015 16:06
Last Modified: 18 Dec 2015 01:00
URI: http://eprints.esc.cam.ac.uk/id/eprint/3478

Actions (login required)

View Item View Item

About cookies