La nappe de Calazaya: une preuve de raccourcissements majeurs gouvernes par des elements paleostructuraux dans les Andes boliviennes

T. Sempere; P. Baby; J. Oller; G. Herail

La nappe de Calazaya: une preuve de raccourcissements majeurs gouvernes par des elements paleostructuraux dans les Andes boliviennes

T. Sempere, P. Baby, J. Oller, G. Herail

Mines Paris - PSL

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

11 Citas (Scopus)

Resumen

A tectonic nappe showing important horizontal displacement is evidenced at the Altiplano-Cordillera Oriental transition in Bolivia (20°S). Its emplacement is related to the eastward transport of a large allochthon domain in the late Oligocene-early Miocene. The basal decollement of the allochthon is located in a stratigraphic unit whose 3-dimensional shape controlled the geometry of deformation. There is an abridged English version. -English summary

Título traducido de la contribución	The Calazaya nappe: evidence for major shortening controlled by paleostructural elements in the Bolivian Andes
Idioma original	Francés
Páginas (desde-hasta)	77-83
Número de páginas	7
Publicación	Comptes Rendus - Academie des Sciences, Serie II
Volumen	312
N.º	1
Estado	Publicada - 1991
Publicado de forma externa	Sí

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abstract = "A tectonic nappe showing important horizontal displacement is evidenced at the Altiplano-Cordillera Oriental transition in Bolivia (20°S). Its emplacement is related to the eastward transport of a large allochthon domain in the late Oligocene-early Miocene. The basal decollement of the allochthon is located in a stratigraphic unit whose 3-dimensional shape controlled the geometry of deformation. There is an abridged English version. -English summary",

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AU - Baby, P.

AU - Oller, J.

AU - Herail, G.

PY - 1991

Y1 - 1991

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AB - A tectonic nappe showing important horizontal displacement is evidenced at the Altiplano-Cordillera Oriental transition in Bolivia (20°S). Its emplacement is related to the eastward transport of a large allochthon domain in the late Oligocene-early Miocene. The basal decollement of the allochthon is located in a stratigraphic unit whose 3-dimensional shape controlled the geometry of deformation. There is an abridged English version. -English summary

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La nappe de Calazaya: une preuve de raccourcissements majeurs gouvernes par des elements paleostructuraux dans les Andes boliviennes

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