The tectonic configuration of northern Patagonia is recognized through geological and geophysical studies, which define several areas characterized by positive and negative gravity anomalies with steep gravity gradients. Positive areas are interpreted as continental crust with Grenvillian and Pampean basement. The Pampean basement occurs to the north and south of the interpreted suture between Patagonia and Gondwana South America. Most negative anomalies are interpreted to represent Gondwana igneous and sedimentary rocks. Areas characterized by steep gravity gradients are coincident with shear zones and mylonitic belts that were active during Gondwana times, a period of great magmatic and tectonic activity in northern Patagonia. Dextral mov...
The southwestern Gondwana basement block configuration in the central Argentinean offshore area was ...
The Preandean geological configuration of the eastern North Patagonian Massif is established through...
Two Early Paleozoic orogenic cycles in the Gondwana margin of NW Argentina were driven by subduction...
Structural analyses in the northern part of the North Patagonia Massif, in the foliated Caita Có gra...
Structural analyses in the northern part of the North Patagonia Massif, in the foliated Caita Có gra...
A multidisciplinary study (U–Pb sensitive high-resolution ion microprobe geochronology, Hf and O iso...
A review of the post-Cambrian igneous, structural and metamorphic history of Patagonia, largely reve...
The origin of Patagonia and its relations with the South American crustal blocks to the north have b...
Structural analyses in the northern part of the North Patagonia Massif, in the foliated Caita Có gra...
AbstractThe Preandean geological configuration of the eastern North Patagonian Massif is established...
This paper analyzes the style, distribution, mechanics and timing of deformation of the Andean retro...
The origin of Patagonia and its relations with the South American crustal blocks to the north have b...
AbstractStructural analyses in the northern part of the North Patagonia Massif, in the foliated Cait...
<p>A multidisciplinary study (U–Pb sensitive high-resolution ion microprobe geochronology, Hf and O ...
The origin of Patagonia and its relations with the South American crustal blocks to the north have b...
The southwestern Gondwana basement block configuration in the central Argentinean offshore area was ...
The Preandean geological configuration of the eastern North Patagonian Massif is established through...
Two Early Paleozoic orogenic cycles in the Gondwana margin of NW Argentina were driven by subduction...
Structural analyses in the northern part of the North Patagonia Massif, in the foliated Caita Có gra...
Structural analyses in the northern part of the North Patagonia Massif, in the foliated Caita Có gra...
A multidisciplinary study (U–Pb sensitive high-resolution ion microprobe geochronology, Hf and O iso...
A review of the post-Cambrian igneous, structural and metamorphic history of Patagonia, largely reve...
The origin of Patagonia and its relations with the South American crustal blocks to the north have b...
Structural analyses in the northern part of the North Patagonia Massif, in the foliated Caita Có gra...
AbstractThe Preandean geological configuration of the eastern North Patagonian Massif is established...
This paper analyzes the style, distribution, mechanics and timing of deformation of the Andean retro...
The origin of Patagonia and its relations with the South American crustal blocks to the north have b...
AbstractStructural analyses in the northern part of the North Patagonia Massif, in the foliated Cait...
<p>A multidisciplinary study (U–Pb sensitive high-resolution ion microprobe geochronology, Hf and O ...
The origin of Patagonia and its relations with the South American crustal blocks to the north have b...
The southwestern Gondwana basement block configuration in the central Argentinean offshore area was ...
The Preandean geological configuration of the eastern North Patagonian Massif is established through...
Two Early Paleozoic orogenic cycles in the Gondwana margin of NW Argentina were driven by subduction...