The Transitional Zone Between the Southern Central and Northern Patagonian Andes (36–39°S)

2015 ◽  
pp. 99-114 ◽  
Author(s):  
Emilio Agustín Rojas Vera ◽  
Darío L. Orts ◽  
Andrés Folguera ◽  
Gonzalo Zamora Valcarce ◽  
Germán Bottesi ◽  
...  
Keyword(s):  
Transitional Zone ◽  
Southern Central ◽  
Patagonian Andes

Tertiary tectonics of the sub-Andean region of the North Patagonian Andes, southern central Andes of Argentina (41–42°30′S)

2005 ◽  
Vol 20 (3) ◽  
pp. 157-170 ◽  
Author(s):  
Raúl E. Giacosa ◽  
Juan C. Afonso ◽  
Nemesio Heredia C. ◽  
José Paredes
Keyword(s):  
Central Andes ◽  
Andean Region ◽  
The North ◽  
Southern Central ◽  
Patagonian Andes

Effects of tectonic deformation and landslides in the erosion of a mountain plateau in the transitional zone between the central and Patagonian Andes

2015 ◽  
Vol 315 (3) ◽  
pp. 257-274 ◽  
Author(s):  
I. M. Penna ◽  
R. L. Hermanns ◽  
S. Daicz ◽  
J. Suriano ◽  
A. M. Tedesco
Keyword(s):  
Transitional Zone ◽  
Tectonic Deformation ◽  
Patagonian Andes

Cenozoic arc-related magmatism in the southern Central and North Patagonian Andes

2019 ◽  
pp. 573-607
Author(s):  
Vanesa D. Litvak ◽  
Lucía Fernández Paz ◽  
Sofía Iannelli ◽  
Stella Poma ◽  
Andrés Folguera
Keyword(s):  
Southern Central ◽  
Patagonian Andes

Analysis and lattice imaging of a transitional event on garnets

1978 ◽  
Vol 36 (1) ◽  
pp. 270-271
Author(s):  
J.Y. Laval
Keyword(s):  
Yttrium Iron Garnet ◽  
Reciprocal Lattice ◽  
Transitional Zone ◽  
Lattice Imaging ◽  
Yttrium Iron ◽  
X Ray ◽  
Ionic Process ◽  
The Matrix ◽  
High Resolution Technique ◽  
Iron Garnet

The exsolution of magnetite from a substituted Yttrium Iron Garnet, containing an iron excess may lead to a transitional event. This event is characterized hy the formation of a transitional zone at the center of which the magnetite nucleates (Fig.1). Since there is a contrast between the matrix and these zones and since selected area diffraction does not show any difference between those zones and the matrix in the reciprocal lattice, it is of interest to analyze the structure of the transitional zones.By using simultaneously different techniques in electron microscopy, (oscillating crystal method microdiffraction and X-ray microanalysis)one may resolve the ionic process corresponding to the transitional event and image this event subsequently by high resolution technique.

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