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International Research<br />

3. Work in progress and future experiments<br />

Interpretation of the signals recovered in August 2008 is presently<br />

in progress. Based on the statistics above, it is expected<br />

that more than 8000 events will be detected and localized by<br />

the MARCHE array during its 3-year deployment period.<br />

Further analysis on the time- and space-distributions of events<br />

over the entire MOMAR area will be conducted as soon as the<br />

three-year catalog is completed and will provide new insights<br />

into active processes along the MOMAR section of the MAR.<br />

Additional work in progress includes a Ph.D. thesis by Abel<br />

Balanche, expected to be completed soon. This work achieved<br />

a 2D finite-element mechanical model of the con<strong>version</strong> process<br />

between seismic and acoustic waves at the seafloor interface.<br />

This model shows that a double-couple source mechanism<br />

produces T-waves which can enter the SOFAR channel with<br />

adequate angles to be trapped into this channel. It also confirms<br />

that a source with a high S-wave content is more efficient<br />

in producing T-waves than a simple explosive source that only<br />

generates P-waves (Balanche et al., 2007). This work will allow<br />

a more accurate determination of earthquake magnitudes from<br />

the amplitudes of the acoustic signals recorded by AUHs.<br />

Further development of AUHs is presently underway in Brest.<br />

The prototype was successfully tested in shallow water in July<br />

2008. We plan to test it in real operational conditions offshore<br />

Villefranche-sur-Mer before the end of this year. After this<br />

second test is completed, a first array of four instruments will<br />

be assembled and deployed at the MARCHE sites in 2009,<br />

thus continuing the monitoring of the MOMAR section of the<br />

MAR at a regional scale.<br />

4. Web sites related to the MARCHE experiment<br />

Additional information on MARCHE, including the preliminary<br />

cruise reports related to the first two deployments, can be<br />

accessed through links from the MARCHE web home page:<br />

http://www-sdt.univ-brest.fr/internet/recherche/Chantiers/<br />

marche. Additional information on MOMAR and previous<br />

acoustic monitoring in the region (the SIRENA and South<br />

Azores arrays) can be found at: http://www.momar.org.<br />

5. Acknowledgments<br />

The scientific parties on board R/V Knorr, R/V Arquipélago,<br />

R/V Le Suroit and NRP Alm. Gago Coutinho wish to thank<br />

the ships’ masters, the officers and crews of these four ships for<br />

their efficient seamanship. The French Ministry of Research<br />

funded ship time for the three cruises sailed aboard Arquipélago<br />

and Le Suroit. The Portuguese Estrutura de Missão para a<br />

Extensão da Plataforma Continental (EMEPC) and its Director,<br />

Pr. M. Pinto De Abreu, secured shiptime on NRP Alm.<br />

Gago Coutinho to sail the MARCHE3/2008 cruise. Salaries<br />

and travel costs were provided by the universities and institutions<br />

to the nationals of the three countries involved. The cost<br />

of developing and building the MARCHE hydrophones, the<br />

deployment costs and the freight costs were shared between<br />

the NOAA Ocean Exploration Program, the French CNRS/<br />

INSU (Institut National des Sciences de l'Univers), and the<br />

MOMAR-France Program.<br />

6. References<br />

Balanche, A., Guennou, C., Goslin, J. and Dziak, R.P., Modeling<br />

of con<strong>version</strong> of seismic to acoustic waves at the seafloor<br />

interface. AGU Fall Meeting. San Francisco, Dec. 2007.<br />

Dziak, R.P., Fox, C.G., Smith, D., et al., Evidence for a probable<br />

magmatic episode at the Lucky Strike segment of the<br />

MAR. Geophys. Res. Abstr., 5, 01784, 2003.<br />

Dziak, R.P., Haxel, J., Bohnenstiehl, D., Goslin, J., Seismicity<br />

rates of slow, intermediate and fast spreading ridges: Insights<br />

from long-term hydroacoustic monitoring. AGU Fall Meeting.<br />

San Francisco, Dec. 2004.<br />

Goslin, J., Martin, C., Perrot, J., et al., Acoustic monitoring<br />

of the Mid-Atlantic Ridge noth of the Azores: Preliminary<br />

results of the SIRENA experiment. <strong>InterRidge</strong> News 13, 9-<br />

13, 2004.<br />

Goslin, J., Lourenço, N., Luis, J., et al., Acoustic monitoring of<br />

the Mid-Atlantic Ridge in the MOMAR Area: Preliminary<br />

results of the ''MARCHE'' experiment. AGU Fall Meeting.<br />

San Francisco, Dec. 2008.<br />

Simão, N., Goslin, J., Perrot, J., Haxel, J. and Dziak, R.P.,<br />

Analysis of the spatial and temporal distribution of the seismicity<br />

of the Mid-Atlantic Ridge using the SIRENA and<br />

the South Azores autonomous hydrophone arrays. AGU Fall<br />

Meeting. San Francisco, Dec. 2006.<br />

Simão, N., Haxel, J., Goslin, J., et al., (in prep.) Characterization<br />

and tectonic implications from seismic sequences along<br />

the northern Mid-Atlantic Ridge (12°N - 47°N) using regional<br />

hydrophone arrays.<br />

For more highlights of research activities at MoMAR,<br />

please refer to the cover image and photos, the national news for France,<br />

and the update from the Monitoring and Observatories Working Group.<br />

www.momar.org<br />

<strong>InterRidge</strong> News 9 Vol. 17, 2008

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