Zobrazeno 1 - 10
of 41
pro vyhledávání: '"Harmegnies, F."'
Publikováno v:
In Marine Geology 2009 261(1):128-137
Publikováno v:
In Marine Geology 2008 247(3):194-207
Autor:
Praeg D., Ceramicola S., Pierre C., Mascle J., Dupré S., Accettella D., Andersen A., Bayon G., Bouloubassi I., Camera L., Cova A., de Lange G., Ducassou E., Duperron S., Freiwald A., Harmegnies F., Hebbeln D., Loncke L., Mastalerz V., Migeon S., Mostafa A., Taviani M., Vanreusel A., Wardell N., BARBIERI, ROBERTO
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______4094::9d046544d10e8b7d05ec10d454f9b177
http://hdl.handle.net/11585/75780
http://hdl.handle.net/11585/75780
Autor:
Praeg D., Ceramicola S., Accettella D., Andersen A., Cova A., Dupré S., Harmegnies F., Mascle J., Pierre C., Unnithan V., Wardell N., BARBIERI, ROBERTO
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______4094::0c837d62d91c7c5617c01dac01213aa7
http://hdl.handle.net/11585/79464
http://hdl.handle.net/11585/79464
Autor:
Dupre, S., Woodside, J.M., Foucher, J.-P., de Lange, G., Mascle, J., Boetius, A., Mastalerz, V., Stadnitskaia, A., Ondreas, H., Huguen, C., Harmegnies, F., Gontharet, S., Loncke, L, Deville, E., Niemann, H., Omoregie, E., Olu-Le Roy, K, Fiala-Medioni, A., Dahlmann, A., Caprais, J.-C., Prinzhofer, A., Sibuet, M., Pierre, C.
Publikováno v:
Deep-Sea Research Part 1. Oceanographic Research Papers, 54(I), 1146-1172. Elsevier Limited
Dupre, S, Woodside, J M, Foucher, J-P, de Lange, G, Mascle, J, Boetius, A, Mastalerz, V, Stadnitskaia, A, Ondreas, H, Huguen, C, Harmegnies, F, Gontharet, S, Loncke, L, Deville, E, Niemann, H, Omoregie, E, Olu-Le Roy, K, Fiala-Medioni, A, Dahlmann, A, Caprais, J-C, Prinzhofer, A, Sibuet, M & Pierre, C 2007, ' Seafloor geological studies of active gas chimneys offshore Egypt (central Nile Fan). ', Deep-Sea Research Part 1. Oceanographic Research Papers, vol. 54, no. I, pp. 1146-1172 . https://doi.org/10.1016/j.dsr.2007.03.007
Dupre, S, Woodside, J M, Foucher, J-P, de Lange, G, Mascle, J, Boetius, A, Mastalerz, V, Stadnitskaia, A, Ondreas, H, Huguen, C, Harmegnies, F, Gontharet, S, Loncke, L, Deville, E, Niemann, H, Omoregie, E, Olu-Le Roy, K, Fiala-Medioni, A, Dahlmann, A, Caprais, J-C, Prinzhofer, A, Sibuet, M & Pierre, C 2007, ' Seafloor geological studies of active gas chimneys offshore Egypt (central Nile Fan). ', Deep-Sea Research Part 1. Oceanographic Research Papers, vol. 54, no. I, pp. 1146-1172 . https://doi.org/10.1016/j.dsr.2007.03.007
Four mud volcanoes of several kilometres diameter named Amon, Osiris, Isis, and North Alex and located above gas chimneys on the Central Nile Deep Sea Fan, were investigated for the first time with the submersible Nautile. One of the objectives was t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::82dcfd8a0f42a7a735e99bc7c5b0cc5f
https://research.vu.nl/en/publications/db17876c-0c76-4833-9c8c-0af623dd7cfd
https://research.vu.nl/en/publications/db17876c-0c76-4833-9c8c-0af623dd7cfd
Publikováno v:
European Brewery Convention: Proceedings Of The 26th Congress Maastricht 1997.
Externí odkaz:
https://doi.org/10.1093/oso/9780199636907.003.0062
Autor:
Auzende, J M, Eissen, J P, Caprais, M P, Gente, P, Gueneley, S, Maze, J P, Harmegnies, F, Lafoy, Y, Lagabrielle, Y
Publikováno v:
Oceanologica Acta, Special issue (0399-1784) (Gauthier-Villars), 1990
The North Fiji Basin (NFB) is a shallow oceanic basin, with depths between 2000 and 4000 m, which lies between latitude 10 degree and 25 degree South and longitude 170 degree and 180 degree East. Situated at the boundary of the Indo-Australian and Pa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_________7::639d362d24d8fc44a7c505780beb2a66
https://archimer.ifremer.fr/doc/00268/37932/
https://archimer.ifremer.fr/doc/00268/37932/
Autor:
Foucher, J P, Bouysse, P, Davagnier, M, Dupont, J, Eissen, J P, Fouquet, Y, Gueneley, S, Harmegnies, F, Lapouille, A
Publikováno v:
Oceanologica Acta, Special issue (0399-1784) (Gauthier-Villars), 1990
The Lau Basin lies between the Lau and Tonga ridges and extends over more than 1000 km. Its width decreases from 300 km near 16 degree S to less than 100 km near 24S. It is an actively spreading oceanic back-arc basin created in the Plio-Pleistocene
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_________7::5550bd79b76a38a09ba26b372f3f5625
https://archimer.ifremer.fr/doc/00268/37933/
https://archimer.ifremer.fr/doc/00268/37933/
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Akademický článek
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