FN Archimer Export Format PT J TI Discovery of continental stretching and oceanic spreading in the Tasman Sea BT AF Lafoy, Y. Géli, Louis Klingelhoefer, Frauke Vially, R. Sichler, Bertrand Nouzé, Herve AS 1:1;2:2;3:2;4:3;5:2;6:2; FF 1:;2:;3:;4:;5:;6:; C1 Direction de l'Industrie, des Mines et de l'Energie, Noumea, Nouvelle-Caledonie Ifremer Centre de Brest, Plouzane, France Institut Francais du Petrole, France C2 DIMENC, FRANCE IFREMER, FRANCE IFP, FRANCE SI BREST IN WOS Ifremer jusqu'en 2018 TC 0 UR https://archimer.ifremer.fr/doc/00210/32141/30598.pdf LA English DT Article CR FAUST1 FAUST2 ZONECO11 BO Unknown L'Atalante AB A deep seismic survey conducted within the western part of New Caledonia's Exclusive Economic Zone (EEZ) (Figure 1) from 8 September–5 October 2004 revealed for the first time the thinned continental and oceanic natures of the crust beneath the eastern Tasman Sea. The survey which was conducted by an international group of scientists a board the Institut Francais de Recherche pour l'Exploitation de la MER (Ifremer) R/V L'Atalante, aimed at improving the understanding of the geological framework, crustal characteristics, and evolution of the submarine basin and ridge system located west of New Caledonia's mainland. The study area, located east of both Australia and the oceanic Tasman Sea Basin, is composed of continental fragments: the Lord Howe Rise and the Norfolk Ridge, which are separated by the New Caledonia and Fairway basins. PY 2005 PD MAR SO Eos, Transactions American Geophysical Union SN 0096-3941 PU Wiley-Blackwell VL 86 IS 10 BP 101 EP 108 DI 10.1029/2005EO100001 ID 32141 ER EF