Influence de l'heritage ante-devonien au front de la chaine andine (Partie centrale de la Bolivie)

D. Zubieta-Rossetti; P. Huyghe; G. Mascle; J. L. Mugnier; P. Baby

Influence de l'heritage ante-devonien au front de la chaine andine (Partie centrale de la Bolivie)

D. Zubieta-Rossetti, P. Huyghe, G. Mascle, J. L. Mugnier, P. Baby

Sección de Ingeniería de Minas

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

2 Citas (Scopus)

Resumen

Seismic profiles on the Eastern front of the Andean belt of Bolivia show pre-existing pre-Devonian thrust structures. The ramp anticlines are located beneath an erosional unconformity at the bottom of the Mesozoic sediments. These pre-Devonian structures are probably late Ordovician or Eocambrian in age and seem to have influenced the distribution of Paleozoic sediments as well as subsequent deformations. The ramps of the pre-Devonian thrust system were slightly reactivated during the Cenozoic migration of the Andean thrust system front. There is an abridged English version. -from English summary

Título traducido de la contribución	The influence of pre-Devonian structures in the development of the front of the Andean Belt, central Bolivia
Idioma original	Francés
Páginas (desde-hasta)	951-957
Número de páginas	7
Publicación	Comptes Rendus - Academie des Sciences, Serie II
Volumen	316
N.º	7
Estado	Publicada - 1993

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title = "Influence de l'heritage ante-devonien au front de la chaine andine (Partie centrale de la Bolivie)",

abstract = "Seismic profiles on the Eastern front of the Andean belt of Bolivia show pre-existing pre-Devonian thrust structures. The ramp anticlines are located beneath an erosional unconformity at the bottom of the Mesozoic sediments. These pre-Devonian structures are probably late Ordovician or Eocambrian in age and seem to have influenced the distribution of Paleozoic sediments as well as subsequent deformations. The ramps of the pre-Devonian thrust system were slightly reactivated during the Cenozoic migration of the Andean thrust system front. There is an abridged English version. -from English summary",

author = "D. Zubieta-Rossetti and P. Huyghe and G. Mascle and Mugnier, \{J. L.\} and P. Baby",

year = "1993",

language = "Franc{\'e}s",

volume = "316",

pages = "951--957",

journal = "Comptes Rendus - Academie des Sciences, Serie II",

number = "7",

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TY - JOUR

T1 - Influence de l'heritage ante-devonien au front de la chaine andine (Partie centrale de la Bolivie)

AU - Zubieta-Rossetti, D.

AU - Huyghe, P.

AU - Mascle, G.

AU - Mugnier, J. L.

AU - Baby, P.

PY - 1993

Y1 - 1993

N2 - Seismic profiles on the Eastern front of the Andean belt of Bolivia show pre-existing pre-Devonian thrust structures. The ramp anticlines are located beneath an erosional unconformity at the bottom of the Mesozoic sediments. These pre-Devonian structures are probably late Ordovician or Eocambrian in age and seem to have influenced the distribution of Paleozoic sediments as well as subsequent deformations. The ramps of the pre-Devonian thrust system were slightly reactivated during the Cenozoic migration of the Andean thrust system front. There is an abridged English version. -from English summary

AB - Seismic profiles on the Eastern front of the Andean belt of Bolivia show pre-existing pre-Devonian thrust structures. The ramp anticlines are located beneath an erosional unconformity at the bottom of the Mesozoic sediments. These pre-Devonian structures are probably late Ordovician or Eocambrian in age and seem to have influenced the distribution of Paleozoic sediments as well as subsequent deformations. The ramps of the pre-Devonian thrust system were slightly reactivated during the Cenozoic migration of the Andean thrust system front. There is an abridged English version. -from English summary

UR - https://www.scopus.com/pages/publications/0027505494

M3 - Artículo

AN - SCOPUS:0027505494

VL - 316

SP - 951

EP - 957

JO - Comptes Rendus - Academie des Sciences, Serie II

JF - Comptes Rendus - Academie des Sciences, Serie II

IS - 7

ER -

Influence de l'heritage ante-devonien au front de la chaine andine (Partie centrale de la Bolivie)

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