FN Archimer Export Format
PT J
TI The jan mayen ridge synthesis of geological knowledge and new data
OT Synthèse dcs connaissances géologiques et données nouvelles sur la ride de Jean Mayen
BT 
AF GAIRAUD, H
   JACQUART, G
   AUBERTIN, F
   BEUZART, Paul
AS 1:1;2:2;3:3;4:4;
FF 1:;2:;3:;4:;
C1 Société Nationale Elf Aquitaine (production). Tour Générale. La Défense 9,92088 Paris La Défense, France
   INST FRANCAIS PETR,F-92500 RUEIL MALMAISON,FRANCE.
   COMPAGNIE FRANCAISE PETR,F-75015 PARIS,FRANCE.
   CTR OCEANOL BRETAGNE,F-29273 BREST,FRANCE.
C2 ELF AQUITAINE, FRANCE
   IFP, FRANCE
   COMPAGNIE FRANCAISE PETR, FRANCE
   COB, FRANCE
IF 0.662
TC 11
UR https://archimer.ifremer.fr/doc/1978/publication-5242.pdf
LA English
DT Article
CR R.V VEMA
   R.V VEMA LEG I CH77
   R.V VEMA LEG II CH78
   R.V VEMA LEG III CH79
BO Jean Charcot
AB The Jan Mayen Ridge and its southern extension were studied by means of multichannel reflection seismic profiles gathered during the Cepan 1 (Cercle Polaire Atlantique Nord) 1975 survey. These data have been interpreted with reference to the evolution of the Norwegian-Greenland Sea, which may be chronologically summarized as follows : 1) opening of the Norwegian basin from the now-extinct Aegir axis 60 myrs ago ( magnetic anomalies 23 to 20) ; 2) westward jumping of the spreading axis : this new axis (Iceland Plateau Extinct Axis) lasted between 5 D and 6 A anomaly times (24 to 18 myrs) ; 3) second westward ridge jump leading to the setting of the currently active Kolbeinsey ridge. [NOT CONTROLLED OCR]
PY 1978
SO Oceanologica Acta
SN 0399-1784
PU Gauthier-villars
VL 1
IS 3
UT A1978FN86500008
BP 335
EP 358
ID 5242
ER

EF