| one publication added to basket [116656] | Geological and biological processes at deep-sea European margins and oceanic basins. International Conference and Eleventh Post-Cruise Meeting of the Training-Through-Research Programme, Bologna, Italy 2-6 February 2003
Marani, M.; Akhmanov, G.; Suzyumov, A.E. (Ed.) (2003). Geological and biological processes at deep-sea European margins and oceanic basins. International Conference and Eleventh Post-Cruise Meeting of the Training-Through-Research Programme, Bologna, Italy 2-6 February 2003. IOC Workshop Report, 187. UNESCO: Paris. 31, II annexes pp.
Deel van: IOC Workshop Report. UNESCO: Paris, meer
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Documenttype: Congres
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Information handling
Surveys > Geological surveys
Topographic features > Submarine features > Continental margins
Water > Deep water
ANE, Europa [Marine Regions]; MED, Europa [Marine Regions]
Marien/Kust |
| Auteurs | | Top |
- Marani, M., redacteur
- Akhmanov, G., redacteur
- Suzyumov, A.E., redacteur
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| Abstract |
The "Geological and biological processes at deep-sea European margins and oceanic basins" - International Conference and 11th Training-through-Research (TTR) Post-Cruise Meeting took place from 2 to 6 February, 2003 at Istituto di Geologia Marina (ISMAR), Area della Ricerca del Consiglio Nazionale delle Ricerche (CNR), Bologna, Italy. The primary focus of the meeting was to discuss the results of the TTR-12 cruise (2002). It brought together participants from eight countries: Belgium, France, Italy, Morocco, Portugal, Russia, Spain and the United Kingdom. Attending were researchers and students with different specialities (sedimentology, geophysics, geochemistry, microbiology, biology, palaeontology, structural geology) and research interests falling in the areas of the conference themes. In total 25 oral presentations and seven poster presentations were made during the meeting that reflect the main research directions of the TTR programme, such as mud volcanism, fluid venting and related prosesses, geosphere-biosphere interactions, tectonics and sedimentation on continental margins and in deep-sea basins. |
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