Matches in DBpedia 2015-10 for { ?s ?p "The Famatinian orogeny (Spanish: Orogenia de Famatina) is a pre-Andean orogeny that took place in western South America during the Paleozoic leading to the formation of the Famatinian orogen also known as the Famatinian belt. The Famatinian orogeny lasted from the Late Cambrian to at least the Late Devonian and possibly the Early Carboniferous with orogenic activity peaking about 490 to 460 million years ago. The Famatinian orogeny led to metamorphism and deformation in the crust and the eruption and intrusion of igneous rock along a Famatinian magmatic arc. The igneous rocks of the Famatinian magmatic arc are of calc-alkaline character and includes gabbros, tonalites and granodiorites. The last and youngest igneous rocks of the arc are granites."@en }
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- Famatinian_orogeny abstract "The Famatinian orogeny (Spanish: Orogenia de Famatina) is a pre-Andean orogeny that took place in western South America during the Paleozoic leading to the formation of the Famatinian orogen also known as the Famatinian belt. The Famatinian orogeny lasted from the Late Cambrian to at least the Late Devonian and possibly the Early Carboniferous with orogenic activity peaking about 490 to 460 million years ago. The Famatinian orogeny led to metamorphism and deformation in the crust and the eruption and intrusion of igneous rock along a Famatinian magmatic arc. The igneous rocks of the Famatinian magmatic arc are of calc-alkaline character and includes gabbros, tonalites and granodiorites. The last and youngest igneous rocks of the arc are granites.".