The Suri Formation is a sedimentary-volcanic succession in the Famatina belt formed during Lower - Middle Ordovician arc magmatism along the western margin of Gondwana. This study reports new lithostratigrafic data relating to the Suri Formation in the Chaschuil valley (Catamarca). The survey defines the main characteristics of volcanism and sedimentation through facies analysis. Epiclastic, volcaniclastic, pyroclastic and peperitic facies were recognized and interpreted in five facies association. The features and relationships of the facies associations indicate environments such as apron volcaniclastic, inner to an outer shelf, and fan distal delta, interbedded with effusive and explosive volcanism. Volcanic activity and relative sea-lev...
This study is focused on the analysis of volcanic deposits that crop out at the middle portion of th...
The granitic rocks of the Sierra de Ancasti represent one of the easternmost outcrops of the Famatin...
The Tunas Formation crops out in the eastern sector of the Ventania System (southwestern Buenos Aire...
The Suri Formation is a sedimentary-volcanic succession in the Famatina belt formed during Lower - M...
The Chuschín formation is a sedimentary-volcanic succession of the Famatina System subduction-relate...
This study is focused on the analyses of a Chaschuil section (27° 49′ S–68° 04′ W), north of the Arg...
The Famatinian arc, over central-western Argentina, is one of the few examples of exposed crustal ar...
In the Central Andes is located one of the major Ordovician basins with fully developed stratigraphi...
The Sistema de Famatina is located in the northwestern sector of Argentina, sharing territories with...
The Early Ordovician granitoids of the Sierra de Velasco reflect the across-arc compositional variat...
In several locations along the Eastern Puna Magmatic Belt (EPMB) porphyritic rhyolite facies are int...
This paper explores the sedimentary provenance of the Ordovician to Devonian siliciclastic sequences...
The 495 to 450 Ma Famatinian orogen, exposed throughout central and northwestern Argentina, formed f...
Six tuffaceous and sandstone levels from an Andean (Mio-Pliocene) synorogenic succession were analyz...
The continental protomargin of Western Gondwana in South America records an important Early-Middle O...
This study is focused on the analysis of volcanic deposits that crop out at the middle portion of th...
The granitic rocks of the Sierra de Ancasti represent one of the easternmost outcrops of the Famatin...
The Tunas Formation crops out in the eastern sector of the Ventania System (southwestern Buenos Aire...
The Suri Formation is a sedimentary-volcanic succession in the Famatina belt formed during Lower - M...
The Chuschín formation is a sedimentary-volcanic succession of the Famatina System subduction-relate...
This study is focused on the analyses of a Chaschuil section (27° 49′ S–68° 04′ W), north of the Arg...
The Famatinian arc, over central-western Argentina, is one of the few examples of exposed crustal ar...
In the Central Andes is located one of the major Ordovician basins with fully developed stratigraphi...
The Sistema de Famatina is located in the northwestern sector of Argentina, sharing territories with...
The Early Ordovician granitoids of the Sierra de Velasco reflect the across-arc compositional variat...
In several locations along the Eastern Puna Magmatic Belt (EPMB) porphyritic rhyolite facies are int...
This paper explores the sedimentary provenance of the Ordovician to Devonian siliciclastic sequences...
The 495 to 450 Ma Famatinian orogen, exposed throughout central and northwestern Argentina, formed f...
Six tuffaceous and sandstone levels from an Andean (Mio-Pliocene) synorogenic succession were analyz...
The continental protomargin of Western Gondwana in South America records an important Early-Middle O...
This study is focused on the analysis of volcanic deposits that crop out at the middle portion of th...
The granitic rocks of the Sierra de Ancasti represent one of the easternmost outcrops of the Famatin...
The Tunas Formation crops out in the eastern sector of the Ventania System (southwestern Buenos Aire...