The Tithonian (Upper Jurassic) ammonite succession at Portada Covunco, Neuquén Mendoza Basin, Argentina

MD simulations in this and previous work has allowed us to propose a relation between the nature of the interactions at the interface and the observed properties of nanofluids:

El área de estudio se localiza sobre la margen izquierda en el tramo inferior del río Limay, dentro del ejido municipal de la ciudad de Plottier (Neuquén, Argentina) y en cercanías

2, localities mentioned in the text; 1, Arroyo de los Patos sur (los Patillos fm.); 2, Alicurá Dam (Nestares fm.); 3, Cañadón la Pintada (Piedra Pintada fm.); 4, Valle del Arroyo

Figure 3. Simplified stratigraphic framework of the Guatá Group in the Paraná State. A, A co-planar surface that represents the initial transgression of the sequence. Note the

They are arranged in recurrent fining upwards sequences composed of the Candeleros, Huincul and Cerro Lisandro formations (Río Limay Subgroup), Portezuelo and Plottier for- mations

Material reviewed: Notoemys oxfordiensis (MNHNCu-P), La Jagua Formation (Upper Jurassic, Oxfordian); Notoemys tlaxiacoensis (IGM-4861), Sabinal Formation (Upper

is here proposed based in its S1 and S2 wide from the base; this sort of suture line differs from other representatives of Spiticeratinae, that have the same elements, where S1

 Investigador del Consejo Nacional de Investigaciones Científicas y Técnicas de la República Argen- tina (CONICET), Unidad IDEHESI-Nodo IH... del Instituto de Fisiografía y