The Hindu Kush slab break-off as revealed by deep structure and crustal deformation.
Kufner, Sofia-Katerina ORCID: https://orcid.org/0000-0002-9687-5455; Kakar, N.; Bezada, M.; Bloch, W.; Metzger, S.; Yuan, X.; Mechie, J.; Ratschbacher, L.; Murodkulov, S.; Deng, Z.; Schurr, B.. 2021 The Hindu Kush slab break-off as revealed by deep structure and crustal deformation. Nature Communications, 12, 1685. 11, pp. https://doi.org/10.1038/s41467-021-21760-w
Before downloading, please read NORA policies.
|
Text (Open Access)
Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/. s41467-021-21760-w.pdf - Published Version Available under License Creative Commons Attribution 4.0. Download (5MB) | Preview |
Abstract/Summary
Break-off of part of the down-going plate during continental collision occurs due to tensile stresses built-up between the deep and shallow slab, for which buoyancy is increased because of continental-crust subduction. Break-off governs the subsequent orogenic evolution but real-time observations are rare as it happens over geologically short times. Here we present a finite-frequency tomography, based on jointly inverted local and remote earthquakes, for the Hindu Kush in Afghanistan, where slab break-off is ongoing. We interpret our results as crustal subduction on top of a northwards-subducting Indian lithospheric slab, whose penetration depth increases along-strike while thinning and steepening. This implies that break-off is propagating laterally and that the highest lithospheric stretching rates occur during the final pinching-off. In the Hindu Kush crust, earthquakes and geodetic data show a transition from focused to distributed deformation, which we relate to a variable degree of crust-mantle coupling presumably associated with break-off at depth.
Item Type: | Publication - Article |
---|---|
Digital Object Identifier (DOI): | https://doi.org/10.1038/s41467-021-21760-w |
ISSN: | 2041-1723 |
Date made live: | 22 Mar 2021 11:51 +0 (UTC) |
URI: | https://nora.nerc.ac.uk/id/eprint/529916 |
Actions (login required)
View Item |
Document Downloads
Downloads for past 30 days
Downloads per month over past year