Sedimentation et structure du bassin de Tipuani-Mapiri: un temoin de l'evolution du front amazonien des Andes du nord de la Bolivie.

M. Fornari; G. Herail; G. Viscara; G. Laubacher; Jaime Argollo Bautista

Sedimentation et structure du bassin de Tipuani-Mapiri: un temoin de l'evolution du front amazonien des Andes du nord de la Bolivie.

M. Fornari, G. Herail, G. Viscara, G. Laubacher, Jaime Argollo Bautista

Resultado de la investigación: Contribución a una revista › Artículo › revisión exhaustiva

8 Citas (Scopus)

Resumen

In the Tipuani-Mapiri basin the Cangalli Formation (Middle to Upper Miocene) partially fossilizes a fluvial erosion paleotopography located in the Amazonian slope of the Cordillera Oriental. The sediments were deposited following the uplift of the Serrania de Carura. This morphotectonic evolution is related to the thrusting activity between the Andean Cordillera and the Sub- Andean belt. Thus, the Cordillera Oriental reliefs appear successively from W to E.-English summary

Título traducido de la contribución	(Sedimentation and structure of the Tipuani- Mapiri basin: a testimony to the Amazonian Front evolution in the Andes of Bolivia) .
Idioma original	Francés
Páginas (desde-hasta)	1303-1308
Número de páginas	6
Publicación	Comptes Rendus de Academie des Sciences, Paris, Serie II
Volumen	305
N.º	16
Estado	Publicada - 1987
Publicado de forma externa	Sí

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title = "Sedimentation et structure du bassin de Tipuani-Mapiri: un temoin de l'evolution du front amazonien des Andes du nord de la Bolivie.",

abstract = "In the Tipuani-Mapiri basin the Cangalli Formation (Middle to Upper Miocene) partially fossilizes a fluvial erosion paleotopography located in the Amazonian slope of the Cordillera Oriental. The sediments were deposited following the uplift of the Serrania de Carura. This morphotectonic evolution is related to the thrusting activity between the Andean Cordillera and the Sub- Andean belt. Thus, the Cordillera Oriental reliefs appear successively from W to E.-English summary",

author = "M. Fornari and G. Herail and G. Viscara and G. Laubacher and {Argollo Bautista}, Jaime",

year = "1987",

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

volume = "305",

pages = "1303--1308",

journal = "Comptes Rendus de Academie des Sciences, Paris, Serie II",

issn = "0249-6305",

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number = "16",

}

Sedimentation et structure du bassin de Tipuani-Mapiri : un temoin de l'evolution du front amazonien des Andes du nord de la Bolivie. / Fornari, M.; Herail, G.; Viscara, G. et al.

En: Comptes Rendus de Academie des Sciences, Paris, Serie II, Vol. 305, N.º 16, 1987, p. 1303-1308.

Resultado de la investigación: Contribución a una revista › Artículo › revisión exhaustiva

TY - JOUR

T1 - Sedimentation et structure du bassin de Tipuani-Mapiri

T2 - un temoin de l'evolution du front amazonien des Andes du nord de la Bolivie.

AU - Fornari, M.

AU - Herail, G.

AU - Viscara, G.

AU - Laubacher, G.

AU - Argollo Bautista, Jaime

PY - 1987

Y1 - 1987

N2 - In the Tipuani-Mapiri basin the Cangalli Formation (Middle to Upper Miocene) partially fossilizes a fluvial erosion paleotopography located in the Amazonian slope of the Cordillera Oriental. The sediments were deposited following the uplift of the Serrania de Carura. This morphotectonic evolution is related to the thrusting activity between the Andean Cordillera and the Sub- Andean belt. Thus, the Cordillera Oriental reliefs appear successively from W to E.-English summary

AB - In the Tipuani-Mapiri basin the Cangalli Formation (Middle to Upper Miocene) partially fossilizes a fluvial erosion paleotopography located in the Amazonian slope of the Cordillera Oriental. The sediments were deposited following the uplift of the Serrania de Carura. This morphotectonic evolution is related to the thrusting activity between the Andean Cordillera and the Sub- Andean belt. Thus, the Cordillera Oriental reliefs appear successively from W to E.-English summary

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M3 - Artículo

AN - SCOPUS:0023503965

VL - 305

SP - 1303

EP - 1308

JO - Comptes Rendus de Academie des Sciences, Paris, Serie II

JF - Comptes Rendus de Academie des Sciences, Paris, Serie II

SN - 0249-6305

IS - 16

ER -

Sedimentation et structure du bassin de Tipuani-Mapiri: un temoin de l'evolution du front amazonien des Andes du nord de la Bolivie.

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