The Salado river basin is the largest one in the Buenos Aires province, with an area near 170,000 km2 . This work aims to perform a stratigraphic analysis of the middle sector of this basin to provide information on the paleoenvironmental evolution during the end of the Quaternary. Results indicate that the evolution of this basin occurred largely in water deficit conditions. Different aeolian lithostratigraphic units are recognized and grouped into three units, as follows: La Postrera, Laguna Las Barrancas, and De la Riestra Formations. New lithological, paleontological, and chronological information is provided regarding the fluvial deposits, which allows for a deeper understanding of the paleoenvironmental conditions that prevailed durin...
This work constitutes an integration of geological, archaeological and palynological data from Santa...
Using an interdisciplinary perspective that integrates archaeological, geomorphological, and palynol...
The main goal of this paper is to analyze the late Quaternary alluvial record of the Andean piedmont...
The regional landscape of the Salado depression is related to weathering, eolian and fluvial process...
The regional landscape of the Salado depression is related to weathering, eolian and fluvial process...
The regional landscape of the Salado depression is related to weathering, eolian and fluvial process...
In the southwestern margin of the Río de la Plata (Argentina), mining works have uncovered deposits ...
The central region of Argentina, southern South America, is characterized by an extensive Quaternary...
The Quequén Salado river basin has been the focus of several contributions since the first decades o...
Se realizó el estudio estratigráfico de detalle de un perfil aflorante en las proximidades de Clarom...
This paper presents a multi-proxy record and its paleoenvironmental interpretation from Pastos Chico...
This paper deals with the way in which the environmental dynamics that took place in the lower basin...
This paper summarizes the available paleoenvironmental information for the Mid-Holocene in Northwest...
The climatic changes that occurred during the late Pleistocene-early Holocene in Patagonia generated...
The Salto de Piedra Paleontological Locality is located in the upper basin of the Tapalqué Creek (Bu...
This work constitutes an integration of geological, archaeological and palynological data from Santa...
Using an interdisciplinary perspective that integrates archaeological, geomorphological, and palynol...
The main goal of this paper is to analyze the late Quaternary alluvial record of the Andean piedmont...
The regional landscape of the Salado depression is related to weathering, eolian and fluvial process...
The regional landscape of the Salado depression is related to weathering, eolian and fluvial process...
The regional landscape of the Salado depression is related to weathering, eolian and fluvial process...
In the southwestern margin of the Río de la Plata (Argentina), mining works have uncovered deposits ...
The central region of Argentina, southern South America, is characterized by an extensive Quaternary...
The Quequén Salado river basin has been the focus of several contributions since the first decades o...
Se realizó el estudio estratigráfico de detalle de un perfil aflorante en las proximidades de Clarom...
This paper presents a multi-proxy record and its paleoenvironmental interpretation from Pastos Chico...
This paper deals with the way in which the environmental dynamics that took place in the lower basin...
This paper summarizes the available paleoenvironmental information for the Mid-Holocene in Northwest...
The climatic changes that occurred during the late Pleistocene-early Holocene in Patagonia generated...
The Salto de Piedra Paleontological Locality is located in the upper basin of the Tapalqué Creek (Bu...
This work constitutes an integration of geological, archaeological and palynological data from Santa...
Using an interdisciplinary perspective that integrates archaeological, geomorphological, and palynol...
The main goal of this paper is to analyze the late Quaternary alluvial record of the Andean piedmont...