Sedimentación sintectónico asociada a las estructuras neógenas en la Precordillera de la zona de Moquella, Tarapacá (19°15′S, norte de Chile)

Luisa Pinto, Gérard Hérail, Reynaldo Charrier

Resultado de la investigación: Article

45 Citas (Scopus)

Resumen

In northern Chile (18-20°S), the western border of the high Andean Plateau (Altiplano) was uplifted by high-angle thrust faults and associated folds. These developed along the Precordillera, which is the morphostructural unit that connects the Andean Plateau, to the east, with the Central Depression, to the west. In the area of Moquella (19.3°S), this structural system is represented by a flexure (Moquella Flexure) and associated syntectonic deposits. The flexure was caused by a blind west-vergent thrust-fault which remained active, at least, between 21 Ma and 16 Ma. It accommodated approximately 700 m of the uplift of the western edge of the Andean Plateau, thereby contributing to 20% of the total uplift. The syntectonic deposits are represented by a 300-400 m thick, Neogene sedimentary and volcanic succession, referred to as Latagualla Formation, exposed in the Central Depression and extending up to the western border of the Precordillera. Part of the Neogene deformation and erosion of the western border of the Andean Plateau was recorded by deposits of this formation. The syntectonic trait of Latagualla Formation is evidenced by growth strata geometries associated with the flexure. In addition, large-scale landslides occurred along the flexural axis, being widely recognized also northward at the latitude of Arica, suggesting a regional extent for these phenomena.

Idioma originalSpanish
Páginas (desde-hasta)19-44
Número de páginas26
PublicaciónRevista Geologica de Chile
Volumen31
N.º1
EstadoPublished - jul 2004

Huella dactilar

flexure
Sedimentation
Neogene
Deposits
plateau
sedimentation
thrust fault
uplift
Landslides
Erosion
landslide
Geometry
fold
erosion
geometry
border

ASJC Scopus subject areas

  • Geology

Citar esto

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title = "Sedimentaci{\'o}n sintect{\'o}nico asociada a las estructuras ne{\'o}genas en la Precordillera de la zona de Moquella, Tarapac{\'a} (19°15′S, norte de Chile)",
abstract = "In northern Chile (18-20°S), the western border of the high Andean Plateau (Altiplano) was uplifted by high-angle thrust faults and associated folds. These developed along the Precordillera, which is the morphostructural unit that connects the Andean Plateau, to the east, with the Central Depression, to the west. In the area of Moquella (19.3°S), this structural system is represented by a flexure (Moquella Flexure) and associated syntectonic deposits. The flexure was caused by a blind west-vergent thrust-fault which remained active, at least, between 21 Ma and 16 Ma. It accommodated approximately 700 m of the uplift of the western edge of the Andean Plateau, thereby contributing to 20{\%} of the total uplift. The syntectonic deposits are represented by a 300-400 m thick, Neogene sedimentary and volcanic succession, referred to as Latagualla Formation, exposed in the Central Depression and extending up to the western border of the Precordillera. Part of the Neogene deformation and erosion of the western border of the Andean Plateau was recorded by deposits of this formation. The syntectonic trait of Latagualla Formation is evidenced by growth strata geometries associated with the flexure. In addition, large-scale landslides occurred along the flexural axis, being widely recognized also northward at the latitude of Arica, suggesting a regional extent for these phenomena.",
keywords = "Central Depression, Flexure, Neogene, Northern Chile, Precordillera, Syntectonic deposits, Uplift of Andean Plateau",
author = "Luisa Pinto and G{\'e}rard H{\'e}rail and Reynaldo Charrier",
year = "2004",
month = "7",
language = "Spanish",
volume = "31",
pages = "19--44",
journal = "Andean Geology",
issn = "0718-7092",
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T1 - Sedimentación sintectónico asociada a las estructuras neógenas en la Precordillera de la zona de Moquella, Tarapacá (19°15′S, norte de Chile)

AU - Pinto, Luisa

AU - Hérail, Gérard

AU - Charrier, Reynaldo

PY - 2004/7

Y1 - 2004/7

N2 - In northern Chile (18-20°S), the western border of the high Andean Plateau (Altiplano) was uplifted by high-angle thrust faults and associated folds. These developed along the Precordillera, which is the morphostructural unit that connects the Andean Plateau, to the east, with the Central Depression, to the west. In the area of Moquella (19.3°S), this structural system is represented by a flexure (Moquella Flexure) and associated syntectonic deposits. The flexure was caused by a blind west-vergent thrust-fault which remained active, at least, between 21 Ma and 16 Ma. It accommodated approximately 700 m of the uplift of the western edge of the Andean Plateau, thereby contributing to 20% of the total uplift. The syntectonic deposits are represented by a 300-400 m thick, Neogene sedimentary and volcanic succession, referred to as Latagualla Formation, exposed in the Central Depression and extending up to the western border of the Precordillera. Part of the Neogene deformation and erosion of the western border of the Andean Plateau was recorded by deposits of this formation. The syntectonic trait of Latagualla Formation is evidenced by growth strata geometries associated with the flexure. In addition, large-scale landslides occurred along the flexural axis, being widely recognized also northward at the latitude of Arica, suggesting a regional extent for these phenomena.

AB - In northern Chile (18-20°S), the western border of the high Andean Plateau (Altiplano) was uplifted by high-angle thrust faults and associated folds. These developed along the Precordillera, which is the morphostructural unit that connects the Andean Plateau, to the east, with the Central Depression, to the west. In the area of Moquella (19.3°S), this structural system is represented by a flexure (Moquella Flexure) and associated syntectonic deposits. The flexure was caused by a blind west-vergent thrust-fault which remained active, at least, between 21 Ma and 16 Ma. It accommodated approximately 700 m of the uplift of the western edge of the Andean Plateau, thereby contributing to 20% of the total uplift. The syntectonic deposits are represented by a 300-400 m thick, Neogene sedimentary and volcanic succession, referred to as Latagualla Formation, exposed in the Central Depression and extending up to the western border of the Precordillera. Part of the Neogene deformation and erosion of the western border of the Andean Plateau was recorded by deposits of this formation. The syntectonic trait of Latagualla Formation is evidenced by growth strata geometries associated with the flexure. In addition, large-scale landslides occurred along the flexural axis, being widely recognized also northward at the latitude of Arica, suggesting a regional extent for these phenomena.

KW - Central Depression

KW - Flexure

KW - Neogene

KW - Northern Chile

KW - Precordillera

KW - Syntectonic deposits

KW - Uplift of Andean Plateau

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M3 - Article

AN - SCOPUS:14844338708

VL - 31

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EP - 44

JO - Andean Geology

JF - Andean Geology

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