UCL Discovery Stage
UCL home » Library Services » Electronic resources » UCL Discovery Stage

The Tethyan Himalayan detrital record shows that India–Asia terminal collision occurred by 54 Ma in the Western Himalaya

Najman, Y; Jenks, D; Godin, L; Boudagher-Fadel, M; Millar, I; Garzanti, E; Horstwood, M; (2017) The Tethyan Himalayan detrital record shows that India–Asia terminal collision occurred by 54 Ma in the Western Himalaya. Earth and Planetary Science Letters , 459 pp. 301-310. 10.1016/j.epsl.2016.11.036. Green open access

[thumbnail of The Tethyan Himalayan detrital record shows that India–Asia terminalcollision occurred by 54Ma in the Western Himalaya.pdf]
Preview
Text
The Tethyan Himalayan detrital record shows that India–Asia terminalcollision occurred by 54Ma in the Western Himalaya.pdf - Published Version

Download (2MB) | Preview

Abstract

The Himalayan orogen is a type example of continent–continent collision. Knowledge of the timing of India–Asia collision is critical to the calculation of the amount of convergence that must have been accommodated and thus to models of crustal deformation. Sedimentary rocks on the Indian plate near the suture zone can be used to constrain the time of collision by determining first evidence of Asian-derived material deposited on the Indian plate. However, in the Himalaya, for this approach to be applied successfully, it is necessary to be able to distinguish between Asian detritus and detritus from oceanic island arcs that may have collided with India prior to India–Asia collision. Zircons from the Indian plate, Asian plate and Kohistan–Ladakh Island arc can be distinguished based on their U–Pb ages combined with Hf signatures. We undertook a provenance study of the youngest detrital sedimentary rocks of the Tethyan Himalaya of the Indian plate, in the Western Himalaya. We show that zircons of Asian affinity were deposited on the Indian plate at 54 Ma. We thus constrain terminal India–Asia collision, when both sutures north and south of the Kohistan–Ladakh Island arc were closed, to have occurred in the Western Himalaya by 54 Ma.

Type: Article
Title: The Tethyan Himalayan detrital record shows that India–Asia terminal collision occurred by 54 Ma in the Western Himalaya
Open access status: An open access version is available from UCL Discovery
DOI: 10.1016/j.epsl.2016.11.036
Publisher version: http://dx.doi.org/10.1016/j.epsl.2016.11.036
Language: English
Additional information: © 2016 The Author(s). Published by Elsevier B.V. This is an open access article under the CC BY license (http://creativecommons.org/licenses/by/4.0/).
Keywords: Himalaya; India–Asia collision; detrital zircon; geochronology; Indus suture zone; Shyok suture zone
UCL classification: UCL
URI: https://discovery-pp.ucl.ac.uk/id/eprint/1540862
Downloads since deposit
5,004Downloads
Download activity - last month
Download activity - last 12 months
Downloads by country - last 12 months

Archive Staff Only

View Item View Item