Signatures of Marsili Seamount Activity from the ORION-GEOSTAR3 Long-Term Seaﬂoor Multiparametric Observatory Experiment

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Signatures of Marsili Seamount Activity from the ORION-GEOSTAR3 Long-Term Seaﬂoor Multiparametric Observatory Experiment

Geophysical Research Abstracts Vol. 12, EGU2010-10274-1, 2010 EGU General Assembly 2010 © Author(s) 2010 Signatures of Marsili seamount activity from the ORION-GEOSTAR3 long-term seafloor multiparametric observatory experiment Angelo De Santis (1,2) and the ORION Team (1) Istituto Nazionale di Geofisica e Vulcanologia, Roma, Italy, (2) Università G. D’Annunzio, Chieti, Italy, (3) IFSI- INAF, Via del Fosso del Cavaliere, 100 (00133) Rome Italy, (4) Eni, Milano, Italy ORION-GEOSTAR3 (EC- 6th FP) has been the first long-term continuous geophysical and oceanographic experiment on the Marsili Seamount, Europe’s largest underwater volcano of Plio-Pleistocenic age. The main scientific objective of this experiment was to detect specific signatures of Marsili activity. A deep sea multiparametric observatory was deployed on the seafloor at the base of the seamount at 3320 m b.s.l., in the period December 2003-May 2005. Among the instruments on board the observatory were: broadband seismometer, hydrophone, gravity meter, magnetometer, water sampler for laboratory analyses, 3D single point current meter, ADCP, CTD and Ph sensor, with a common accurate time reference. Multiparametric analysis shows that data are generally of good quality, showing continuous time series with only a very few gaps. Seismic, chemical, oceanographic, magnetic, and gravity data were analysed both in the time and frequency do- mains. This presentation will show some examples of analyses and comparisons. For instance, both the analysis of individual time series and their comparison have already shown interesting results: estimation of the lithospheric depth under the Marsili, lateral attenuation distribution of recorded seismic body waves and indications for possi- ble existence of a hydrothermal circuit. Significant correlations between recorded time series could be related to activity and structure of the Marsili seamount revealing interesting and unknown characteristics of this submarine volcano..

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