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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