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Many of the designations used by the manufacturers and sellers to promote their products are claimed as trademarks. Where those designation appear in the Report and ISMAR-CNR was aware of a trademark claim the designations have been printed in all caps. In addition, we have reported some of them in the Production Notes below in this page and in the ACRONYM table thereinafter. Nothing in this document is meant to imply any endorsement or recommendation, positive or negative, concerning any systems or programs mentioned herein. The data presented hereafter is the property of CNR and of the Joint Research Program. Unauthorized use of the data would be considered unfair. Many of the systems and programs used to generate data are 'free' because either they are either public domain or the licences are roughly equivalent to the GNU Public License. Some programs are either commercial or have more restrictive licenses and may require payment. Where known, programs and systems that are not `free' are acknowledged.
ISMAR-CNR Cataloging-In-Publication data: ISMAR Bologna TECHNICAL REPORT
Marm2009: marine geological study Of The North Anatolian Fault beneath The Sea Of Marmara. Ec Esonet Marmara Demo Mission, R/V Urania, Cruise Report.
by Gasperini L., Geli L., Favali P., Çagatay N., Görür N., Bortoluzzi G., Del Bianco F., Kuruoglu E., Romano S., Etiope G., Innocenzi L., Marinaro G., Approioul R., Le Piver D., Pelleau P., Roudaut M., Acar D., Akarsu E., Akkok R., Biltekin D., Can A., Elbeck S., Ozmaral A., Ozeren S., Sancar E., Ulgen U., Cefalogli L, Veditti V..
Includes bibliographical reference and index.
1. tectonics 2. active faults 3. paleoseismology 4. seismology 5. Sea of Marmara
Abstract - A marine geological cruise, MARMARA2009, was carried out in the frame of MARM-ESONET, a demo mission of the EC funded ESONET Network of Excellence (European Seafloor Observatory Network). Main objective of the project was the attempting to assess and mitigate seismic hazards in the region close to Istanbul through geological/geophysical surveys carried out in the Sea of Marmara along the submerged track of the North Anatolian Fault and the deployment of seafloor observatories. During MARMARA2009 we collected multibeam bathymetry, side-scan sonar imagery and chirp sub-bottom data, together with carefully positioned core samples. A submarine station of the GEOSTAR family (SN-4), 10 OBS and 5 piezometers were deployed on bottom, for recording periods up to 1 year. Although selected prior of the cruise, the SN4-observatory site has been surveyed before deployment with geophysical imaging techniques and direct groundthruting with a deep towed system, the MEDUSA, that provided oceanographic data (CTD), methane content in the water column and visual inspection through a high-resolution video camera.
Sommario - Vengono presentati le metodologie e l'insieme dei risultati ottenuti durante la campagna MARM2009 di rilievi geofisici, geologici e oceanografici nel Mar di Marmara. E' stata utilizzata la nave da ricerca R/V Urania del CNR,
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Copyright © 2009 by ISMAR-CNR - Via Gobetti 101 40129 Bologna, Italy.
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Section 1 gives the introductory and background information, including some technological and scientific issues of the organization and execution of tasks, whereas section 2 summarizes the cruise operations. Section 3 provides the technical aspects that were involved in the data acquisition and processing. Sections 4 and following discuss the initial results, the on-going data processing and usage, and give concluding remarks. Some data processing procedures that were used in the production of this report along with additional technical details and data are presented in the Appendix.
Many people contributed to the success of the research cruise (MARM09 R/V Urania). We are particularly indebted to the Captain Emanuele Gentile, the officers and crew members of R/V Urania for their professionalism and efforts in assuring the success of the cruise. Turkish SHOD is warmly acknowledged for support and encouragement. The project was co-funded by Italian CNR and EU's ESONET.