FN Archimer Export Format
PT J
TI Bay of biscay and Pyrenees
BT 
AF CHOUKROUNE, Pierre
   LE PICHON, Xavier
   SEGURET, Michel
   SIBUET, Jean-Claude
AS 1:;2:;3:;4:;
FF 1:;2:;3:;4:;
TC 0
UR https://archimer.ifremer.fr/doc/1973/publication-5061.pdf
LA English
DT Article
DE ;Histoire Ifremer
AB The different hypotheses proposed for the creation of the Bay of Biscay are reviewed. New geological and geophysical data collected in the last two years in the Bay and in the Pyrenean domain give new insight into the tectogenesis of the Pyrenees.  Geological data of the Pyrenean area provide tight constraints on the hypothesis of formation of the Bay. The most probable hypothesis is an opening by rotation of the Iberian Peninsula around a pole of rotation situated near Paris, which resulted in strike-slip motion dong the North Pyrenean fault during the Upper Mesozoic.  A progressive westward migration of the pole initiated in the late Cretaceous blocked the motion dong the fault and led to the main Eocene tectogenetic Pyrenean phase. [NOT CONTROLLED OCR]
PY 1973
SO Earth and Planetary Science Letters
PU North- Holland Publishing Company
VL 18
BP 109
EP 118
ID 5061
ER

EF