OLIGOCENE-NEOGENE TECTONIC EVOLUTION OF THE ALTIPLANO OF NORTHERN CHILE (18-19°8)
Texte intégral
Documents relatifs
– LSI boxplots for small size camelids from Early Archaic site Tambillo-1, Late Archaic sites (Puripica-1 and Tulá-52), and Early Formative sites located at Quebrada Tulán (Tulán-54,
En unidades del Mioceno temprano, correspondientes a la Formación Centinela en la zona de lago Buenos Aires, Formación Río Jeinemeni y Formación Santa Cruz, representan el 15% de la
Jurassic to Early Cretaceous rocks from the Coastal Cordillera and Cretaceous to Paleocene rocks from the Central Depression show similar magnitude (>30) clockwise rotations,
The alongshore wind stress near the coast was found to play a role in forcing the annual component of the seasonal cycle of the thermocline depth, but the important
- Five facies associations, which form the bulk of the Atacama Gravels along the Chañaral- Pedernales transect, indicate sedimentary processes on alluvial fan, ephemeral fluvial
In particular, the intriguing interplay between external parameters (electric fi eld, strain) and band structure, as well as the basic properties of heterostructures formed
The Pvull - SamH1147 bp fragment derived from exon 4 of the granzyme H gene (44% nucleotide identities with the homologous granzyme B sequence) was used as a highly specific,
[Mortimer y Saric, 1975], y su acumulación habría tenido lugar previo al alzamiento de la Cordillera de la Costa; ii) Depósitos marinos de Sierra del Ancla,