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Details of Award

NERC Reference : NER/B/S/2003/00174

The causes and significance of crustal melting, southern Tibet.

Grant Award

Principal Investigator:
Professor NB Harris, The Open University, Environment, Earth & Ecosystems
Co-Investigator:
Professor RR Parrish, University of Portsmouth, Sch of the Env, Geography & Geosciences
Co-Investigator:
Dr T Argles, The Open University, Faculty of Sci, Tech, Eng & Maths (STEM)
Science Area:
Earth
Overall Classification:
Earth
ENRIs:
Global Change
Science Topics:
Tectonic Processes
Properties Of Earth Materials
Climate & Climate Change
Abstract:
This project will elucidate the thermal and rheological evolution of the crust during tectonic thickening in the hinterland of the Himalayan orogen and assess constraints on surface uplift rates. Combined field and geochemical studies of mid-Miocene granites and dykes intruding a >1000 km-long, crustal-scale antiform south of the Tsangpo suture zone will (i) provide insights into deeper crustal processes than have been deduced from the High Himalayan granites to the south, and (ii) assess the role of the controversial 'partial melt zone' in the mid-crust inferred from seismic imaging. Detailed mapping coupled with accessory-phase chronometry, Sr-Nd isotope systematics and Ar-Ar cooling age profiles will determine the source of crustal melts and the relative timing of anatexis, doming and thrusting, thus identifying the causes of magmatism in this crucial part of the collision zone.
Period of Award:
1 Oct 2003 - 30 Sep 2005
Value:
£19,744
Authorised funds only
NERC Reference:
NER/B/S/2003/00174
Grant Stage:
Completed
Scheme:
Small Grants Pre FEC
Grant Status:
Closed
Programme:
Small Grants

This grant award has a total value of £19,744  

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FDAB - Financial Details (Award breakdown by headings)

Total - T&STotal - Other Costs
£10,518£9,226

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