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Water in the Earth s lithosphere and its bearing on geophysical properties

This application relates to the water (i.e., H+, OH-, H2O) distribution in the Earth's lithosphere and its bearing on the Earth’s geophysical properties. The aim of this proposal is to explore the distribution of water in the lith... ver más

30/04/2013

MFGI

100K€

Presupuesto del proyecto: 100K€

Líder del proyecto

MAGYAR FOLDTANI ES GEOFIZIKAI INTEZET No se ha especificado una descripción o un objeto social para esta compañía.

TRL 4-5

Fecha límite participación Sin fecha límite de participación.

Financiación concedida El organismo FP7 notifico la concesión del proyecto el día 2013-04-30 No tenemos la información de la convocatoria

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Información adicional privada

No hay información privada compartida para este proyecto. Habla con el coordinador.

1 Participantes

MFGI

0.00€ | Lider

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Líder del proyecto

MAGYAR FOLDTANI ES GEOFIZIKAI INTEZET No se ha especificado una descripción o un objeto social para esta compañía.

TRL 4-5

Presupuesto del proyecto 100K€

Fecha límite de participación Sin fecha límite de participación.

Descripción del proyecto This application relates to the water (i.e., H+, OH-, H2O) distribution in the Earth's lithosphere and its bearing on the Earth’s geophysical properties. The aim of this proposal is to explore the distribution of water in the lithosphere and understand its effect on the geophysical properties (seismic and electric conductivity) of lithospheric rocks. This development has the potential to provide a better insight into the rheology and dynamics of the Earth’s lithosphere, and may facilitate assessment of the risk of earthquakes. This is because water is known to weaken minerals even at very low concentration levels (ppm). There are basaltic volcanoes in the Carpathian-Pannonian region, which sampled the Earth’s lithosphere by picking up rocks from the lithosphere (i.e., xenoliths) during their eruption. More importantly, some of these xenolith bearing basaltic volcanoes sit close to geophysical cross-sections which provides an extraordinary chance to correlate geophysical measurements against xenoliths and their water concentration. A new, revolutionary infrared method currently discovered at the Research School of Earth Sciences in Australia will be utilized by the Eotvos Lorand Geophysical Institute in Hungary which will allow a much simpler analysis of a large number of xenoliths for water. The aims of the proposal are the following: 1) Study diffusion profiles of water in xenoliths to reveal their representativity for the source region 2) Understanding the distribution of water in the lithosphere; 3) To improve geophysical models by integrating the newly emerging information on water distribution in mantle rocks into already existing seismic databases.

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