Consulta: creatorFacets:"Lapouille, A"
Registros recuperados: 3
Data/hora: 03/06/2024 05:42:51

Age and origin of the sea-floor of the banda sea (eastern indonesia)
Provedor de dados: 5
Autores: Lapouille, A; Haryono, H; Larue, M; Pramumijoyo, S; Lardy, M.
Tipo: Text
Ano: 1985
URL: http://archimer.ifremer.fr/doc/00112/22285/19960.pdf

Accrétion océanique et déformation dans la partie méridionale du bassin Nord-Fidjien: résultats préliminaires de la campagne océanographique SEAPSO III du N.O. Jean-Charcot (décembre 1985)
Provedor de dados: 5
Autores: Auzende, Jean-marie; Eissen, Jean-philippe; Caprais, Marie-paule; Gente, Pascal; Gueneley, S; Harmegnies, Francois; Lagabrielle, Yves; Lapouille, A; Lefevre, C; Maillet, P; Maze, Jean-pierre; Ondreas, Helene; Schaaf, A; Singh, R.
Seismic, Seabeam, magnetic and gravimetrie surveys in the southern part of the N-Fiji basin were conducted during the SEAPSO LEG III Cruise. The active spreading axis was recognized between 17°30'S and 21°S. It consists of a continuous N-S Ridge cross-cut by transverse directions oriented N25 and N45. North of 17°30'S, the spreading System is more complex due to the existence of a possible triple junction located around 15° S. The eastern part of the N-Fiji basin, west of Viti Levu is mostly characterized by alternating highs and deeps (&lt;4,000 m). This area must be regarded no more as a spreading center, but as complex boundary suffering transverse tectonics.
Tipo: Text
Ano: 1986
URL: http://archimer.ifremer.fr/doc/00184/29492/27835.pdf

Campagne Seapso 4: Etude morphostructurale de la ride de Valufa dans le bassin de Lau
Provedor de dados: 5
Autores: Foucher, J P; Bouysse, P; Davagnier, M; Dupont, J; Eissen, J P; Fouquet, Y; Gueneley, S; Harmegnies, F; Lapouille, A.
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 the Tonga Trench. The part of the Valu Fa ridge North of 22 degree S was investigated during the Seapso 4 cruise of R/V Jean Charcot in Jan 1986 and complementary data were obtained during the Papnoum transit (Apr 1987). The techniques used included multibeam bathymetry, single-channel seismic reflection, magnetic and gravity field measurements.
Tipo: Text
Ano: 1990
URL: http://archimer.ifremer.fr/doc/00268/37933/36014.pdf