SciELO - Scientific Electronic Library Online

 
vol.26 número1Variaciones en indicadores geoquímicos (tierras raras e isótopos estables de carbono) en relación con la paleoprofundidad: ejemplos de depósitos marinos de las cuencas Neuquina y AustralRevisión de la estratigrafía Eocena-Pliocena de la cuenca intermontana de San Antonio de los Cobres, Puna Salteña, Argentina índice de autoresíndice de materiabúsqueda de artículos
Home Pagelista alfabética de revistas  

Servicios Personalizados

Revista

Articulo

Indicadores

  • No hay articulos citadosCitado por SciELO

Links relacionados

  • No hay articulos similaresSimilares en SciELO

Compartir


Latin American journal of sedimentology and basin analysis

versión On-line ISSN 1851-4979

Resumen

LOPEZ STEINMETZ, Romina L  y  MONTERO-LOPEZ, Carolina. Stratigraphy and sedimentary environments of the Villa María and Peña Colorada formations (paleogene), westernmost Argentine plateau. Lat. Am. j. sedimentol. basin anal. [online]. 2019, vol.26, n.1, pp.39-56. ISSN 1851-4979.

The Peña Colorada Formation records the early stage of Andean foreland sedimentation over ~1,000 km2 in the north westernmost Argentine plateau (21°51’ S - 66°12’ W). The aim of the present contribution is to provide a detailed stratigraphic characterization of these deposits and the description of their sedimentary environments. Detailed stratigraphic observations conducted to the division of the Peña Colorada Formation in two formal units, the Villa María and Peña Colorada formations. Subsequently, these two formations were divided into members according to sedimentary facies, textural tendencies, the alternating presence of quartz, carbonate and gypsum veins, and the distinctive cementation of deposits by iron carbonate, silica, and calcium carbonate. Data suggest that sedimentation would have taken place in alluvial plains near sourcing sediments that were being actively uplifted.

Palabras clave : Eocene; Oligocene; Sedimentary basin; Andean Plateau.

        · texto en Inglés     · Inglés ( pdf )

 

Creative Commons License Todo el contenido de esta revista, excepto dónde está identificado, está bajo una Licencia Creative Commons