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Details of Award

NERC Reference : NER/A/S/2000/01008

Timescales and mechanisms of generating silicic magmas: the clues are in the crystals.

Grant Award

Principal Investigator:
Professor J Davidson, Durham University, Earth Sciences
Science Area:
None
Overall Classification:
Earth
ENRIs:
Global Change
Environmental Risks and Hazards
Science Topics:
Volcanic Processes
Properties Of Earth Materials
Geohazards
Abstract:
Understanding the mechanisms by which large silicic magma bodies are produced is critical to hazard prediction in regions of rhyolite volcanism, and is an important constraint on crustal growth and differentiation models. The crystals contained in silicic rocks contain a record of the evolution of the magma in which they grew or were dispersed. Therefore, a detailed analysis of the crystals - in particular core-rim isotopic profiles - will enable us to obtain a far clearer picture of the source of silicic magmas and how they differentiate. The Taupo, Fish Canyon and Bishop magma systems, considered representative of the spectrum of large silicic volcanic systems, will form the focus of this study. The fundamental analytical techniques have been developed by the PI. PDRA Bruce Charlier will bring his experience in detailed isotopic microanalysis on silicic rocks.
Period of Award:
1 Aug 2001 - 31 Jul 2004
Value:
£161,144
Authorised funds only
NERC Reference:
NER/A/S/2000/01008
Grant Stage:
Completed
Scheme:
Standard Grants Pre FEC
Grant Status:
Closed
Programme:
Standard Grant

This grant award has a total value of £161,144  

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FDAB - Financial Details (Award breakdown by headings)

Total - T&STotal - StaffTotal - Other CostsTotal - Indirect CostsTotal - Equipment
£5,509£75,020£6,809£34,509£39,298

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