Role des paleostructures albo-cenomaniennes dans la geometrie des chevauchements frontaux nord-pyreneens.

P. Baby; G. Crouzet; M. Specht; J. Deramond; M. Bilotte; E. J. Debroas

Role des paleostructures albo-cenomaniennes dans la geometrie des chevauchements frontaux nord-pyreneens.

P. Baby
, G. Crouzet
, M. Specht
, J. Deramond
, M. Bilotte
, E. J. Debroas

GET-UMR CNRS/IRD/Univ. Paul Sabatier

Producción científica: Contribución a una revista › Artículo › revisión exhaustiva

20 Citas (Scopus)

Resumen

The N Pyrenean Zone is moved N by a major S dipping thrust, which dies out in the N Pyrenean Frontal Thrusts. Balanced cross- sections and recent sedimentologic data show N Pyrenean Frontal Thrust geometry is led by fault scarps, bounding previous Albo-Cenomanian basins. There is an abridged English version.-English summary

Título traducido de la contribución	(Role of Albo-Cenomanian paleostructures in the geometry of North- Pyrenean frontal thrusts).
Idioma original	Francés
Páginas (desde-hasta)	307-313
Número de páginas	7
Publicación	Comptes Rendus - Academie des Sciences, Serie II
Volumen	306
N.º	4
Estado	Publicada - 1988
Publicado de forma externa	Sí

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title = "Role des paleostructures albo-cenomaniennes dans la geometrie des chevauchements frontaux nord-pyreneens.",

abstract = "The N Pyrenean Zone is moved N by a major S dipping thrust, which dies out in the N Pyrenean Frontal Thrusts. Balanced cross- sections and recent sedimentologic data show N Pyrenean Frontal Thrust geometry is led by fault scarps, bounding previous Albo-Cenomanian basins. There is an abridged English version.-English summary",

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AU - Baby, P.

AU - Crouzet, G.

AU - Specht, M.

AU - Deramond, J.

AU - Bilotte, M.

AU - Debroas, E. J.

PY - 1988

Y1 - 1988

N2 - The N Pyrenean Zone is moved N by a major S dipping thrust, which dies out in the N Pyrenean Frontal Thrusts. Balanced cross- sections and recent sedimentologic data show N Pyrenean Frontal Thrust geometry is led by fault scarps, bounding previous Albo-Cenomanian basins. There is an abridged English version.-English summary

AB - The N Pyrenean Zone is moved N by a major S dipping thrust, which dies out in the N Pyrenean Frontal Thrusts. Balanced cross- sections and recent sedimentologic data show N Pyrenean Frontal Thrust geometry is led by fault scarps, bounding previous Albo-Cenomanian basins. There is an abridged English version.-English summary

UR - https://www.scopus.com/pages/publications/0023796422

M3 - Artículo

AN - SCOPUS:0023796422

VL - 306

SP - 307

EP - 313

JO - Comptes Rendus - Academie des Sciences, Serie II

JF - Comptes Rendus - Academie des Sciences, Serie II

IS - 4

ER -

Role des paleostructures albo-cenomaniennes dans la geometrie des chevauchements frontaux nord-pyreneens.

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