FAULTING PROCESS OF A PRESTRUCTURED PASSI VE MARGIN - THE GULF OF LIONS (NORTHWESTERN MEDITERRANEAN-SEA)

Citation
P. Viallard et C. Gorini, FAULTING PROCESS OF A PRESTRUCTURED PASSI VE MARGIN - THE GULF OF LIONS (NORTHWESTERN MEDITERRANEAN-SEA), Comptes rendus de l'Academie des sciences. Serie II. Mecanique, physique, chimie, astronomie, 319(5), 1994, pp. 567-572
Citations number
15
Categorie Soggetti
Multidisciplinary Sciences
ISSN journal
12518069
Volume
319
Issue
5
Year of publication
1994
Part
2
Pages
567 - 572
Database
ISI
SICI code
1251-8069(1994)319:5<567:FPOAPP>2.0.ZU;2-1
Abstract
Tectonic study of a passive margin necessitates distinction between st ructures linked to the initial stretching of the crust and gravitation al structures; In the Gulf of Lions, initial extension in the Oligocen e to Early Aquitanian has produced an asymmetric system of horsts and grabens. Major faults, plunging southeast, are inherited from Late-Her cynian or Mesozoic faults and from Eocene thrusts. Gravitational struc tures are either early structures following the rifting event or late structures linked to thermal subsidence.