This Special Issue gathers together a series of contributions related to the Famatinian orogen in the South American plate. This orogen was initially defined in northwestern Argentina by Aceñolaza and Toselli (1976) and is currently understood as a subduction-related accretionary orogen that was formed during the Ordovician. It extends along the proto-Andean margin of Gondwana from Venezuela to Patagonia (Cawood et al., 2009). Magmatism took place mostly between c. 490 and 460 Ma along the entire proto-margin, suggesting global geodynamics as the prime controlling factor. Recently, Rapela et al. (2018) published a detailed isotope-geochemical review of Famatinian magmatism in the Argentinean Sierras Pampeanas where its areal exte...
Trabajo presentado en el XV Congreso Geológico Chileno, celebrado en Concepción (Chile), del 18 al 2...
In this classic segment, many tectonic processes, like flat-subduction, terrane accretion and steepe...
The Early Ordovician granitoids of the Sierra de Velasco reflect the across-arc compositional variat...
Along the proto-Pacific margin of Gondwana, from Venezuela to northeastern Patagonia, the Early–Midd...
Along the proto-Pacific margin of Gondwana, from Venezuela to northeastern Patagonia, the Early–Midd...
The continental protomargin of Western Gondwana in South America records an important Early-Middle O...
Along the proto-Pacific margin of Gondwana, from Venezuela to northeastern Patagonia, the Early–Midd...
The Famatinian arc, over central-western Argentina, is one of the few examples of exposed crustal ar...
The Famatinian is a segment of the Ordovician Terra Australis accretionary orogen that stretched alo...
We studied the P-T-t evolution of a mid-crustal igneous-metamorphic segment of the Famatinian Belt i...
Two Early Paleozoic orogenic cycles in the Gondwana margin of NW Argentina were driven by subduction...
The Pampia cratonic block is juxtaposed to the Paleoproterozoic Río de la Plata craton through the C...
New SHRIMP U–Pb zircon and monazite ages from the Sierra de Fiambalá (Sierras Pampeanas, NW Argentin...
Along the proto-Pacific margin of Gondwana, from Venezuela to northeastern Patagonia, the Early–Midd...
New petrologic, thermobarometric and U-Pb monazite geochronologic information allowed to resolve the...
Trabajo presentado en el XV Congreso Geológico Chileno, celebrado en Concepción (Chile), del 18 al 2...
In this classic segment, many tectonic processes, like flat-subduction, terrane accretion and steepe...
The Early Ordovician granitoids of the Sierra de Velasco reflect the across-arc compositional variat...
Along the proto-Pacific margin of Gondwana, from Venezuela to northeastern Patagonia, the Early–Midd...
Along the proto-Pacific margin of Gondwana, from Venezuela to northeastern Patagonia, the Early–Midd...
The continental protomargin of Western Gondwana in South America records an important Early-Middle O...
Along the proto-Pacific margin of Gondwana, from Venezuela to northeastern Patagonia, the Early–Midd...
The Famatinian arc, over central-western Argentina, is one of the few examples of exposed crustal ar...
The Famatinian is a segment of the Ordovician Terra Australis accretionary orogen that stretched alo...
We studied the P-T-t evolution of a mid-crustal igneous-metamorphic segment of the Famatinian Belt i...
Two Early Paleozoic orogenic cycles in the Gondwana margin of NW Argentina were driven by subduction...
The Pampia cratonic block is juxtaposed to the Paleoproterozoic Río de la Plata craton through the C...
New SHRIMP U–Pb zircon and monazite ages from the Sierra de Fiambalá (Sierras Pampeanas, NW Argentin...
Along the proto-Pacific margin of Gondwana, from Venezuela to northeastern Patagonia, the Early–Midd...
New petrologic, thermobarometric and U-Pb monazite geochronologic information allowed to resolve the...
Trabajo presentado en el XV Congreso Geológico Chileno, celebrado en Concepción (Chile), del 18 al 2...
In this classic segment, many tectonic processes, like flat-subduction, terrane accretion and steepe...
The Early Ordovician granitoids of the Sierra de Velasco reflect the across-arc compositional variat...