GLOBALSEIS

NEW GOALS AND DIRECTIONS FOR OBSERVATIONAL GLOBAL SEISMOLOGY

Coordinatore	CENTRE NATIONAL DE LA RECHERCHE SCIENTIFIQUE    more Spiacenti, non ci sono informazioni su questo coordinatore. Contattare Fabio per maggiori infomrazioni, grazie.
Nazionalità Coordinatore	France [FR]
Totale costo	2˙500˙000 €
EC contributo	2˙500˙000 €
Programma	FP7-IDEAS-ERC Specific programme: "Ideas" implementing the Seventh Framework Programme of the European Community for research, technological development and demonstration activities (2007 to 2013)
Code Call	ERC-2008-AdG
Funding Scheme	ERC-AG
Anno di inizio	2009
Periodo (anno-mese-giorno)	2009-02-01   -   2015-01-31

 Partecipanti

#	participant	country	role	EC contrib. [€]
1	CENTRE NATIONAL DE LA RECHERCHE SCIENTIFIQUE  Organization address address: Rue Michel -Ange 3 city: PARIS postcode: 75794 contact info Titolo: Ms. Nome: Béatrice Cognome: Saint-Cricq Email: send email Telefono: +33 4 93 95 42 22 Fax: +33 4 92 96 03 39	FR (PARIS)	hostInstitution	2˙500˙000.00
2	CENTRE NATIONAL DE LA RECHERCHE SCIENTIFIQUE  Organization address address: Rue Michel -Ange 3 city: PARIS postcode: 75794 contact info Titolo: Prof. Nome: Augustinus Cognome: Nolet Email: send email Telefono: -92942603 Fax: -92942581	FR (PARIS)	hostInstitution	2˙500˙000.00

Mappa

 Word cloud

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 Obiettivo del progetto (Objective)

'One of the major paradoxes in the geosciences is the contrast between the geochemical evidence for limited mass-exchange between lower and upper mantle, and the geophysical arguments for significant mass exchange, needed to prevent the mantle from melting in the geological past. Seismic tomography, when ultimately combined with geodynamical modeling, needs to provide estimates of present-day flux. Indeed, tomography has shown evidence for slabs penetrating into the lower mantle; but no quantitative information on the degree of mass exchange and heat flux can, as yet, reliably be obtained from tomographic images. It is crucial that the boundary between upper- and lower mantle be imaged at greater precision, certainly in the plume-rich southern hemisphere. This requires a combined effort of improvements both experimentally and theoretically. Much progress has recently been obtained by my group in Princeton before I returned to Europe. I propose to build upon those accomplishments, and to (1) Expand the data acquisition to the oceans by developing hydrophone-equipped floats, with the goal to improve data coverage in regions that are important to investigate heat flux: the plume-rich southern hemisphere in particular, (2) Combine different seismological data sets spanning a wide range of frequencies, with the goal to obtain tomographic images that allow for a quantitative estimate of heat flux (both upwards through plumes and downwards through the sinking of slab fragments), with emphasis on the boundary between upper- and lower mantle, (3) Exploit the extra resolution offered by the frequency-dependent sensitivity of body waves (multifrequency tomography), (4) Incorporate wavelet expansions into the tomographic inversion, with the aim to resolve more detail in the model where the data allow a higher resolution, (5) Obtain a multidisciplinary interpretation of new tomographic results through interaction with geodynamicists and geochemists.'