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The Andean orogeny (Spanish: Orogenia andina) is an ongoing process of orogeny that began in the Early Jurassic and is responsible for the rise of the Andes mountains. The orogeny is driven by a reactivation of a long-lived subduction system along the western margin of South America. On a continental scale the Cretaceous (90 Ma) and Oligocene (30 Ma) were periods of re-arrangements in the orogeny. Locally the details of the nature of the orogeny varies depending on the segment and the geological period considered.

AttributesValues
type
label
  • Andean orogeny
  • Andinska orogenesen
  • Orogenesi andina
  • Orogenia andina
  • Андська складчастість
  • 安第斯造山運動
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  • L'orogenesi andina è un processo orogenetico tuttora in corso che ebbe inizio nel Giurassico inferiore e che ha dato luogo alla formazione delle Ande. L'orogenesi è legata alla riattivazione di un antico sistema subduttivo lungo il margine occidentale del Sud America. Il Cretacico (90 milioni di anni fa) e l'Oligocene (30 milioni di anni fa) furono periodi di riarrangiamento orogenetico su scala continentale. A livello locale i dettagli e la natura dell'orogenesi variano in funzione del segmento e del periodo considerato.
  • La orogenia andina es un proceso de orogénesis responsable del alzamiento de la Cordillera de los Andes y que viene actuando desde el Jurásico hasta el presente. La orogenia es la consecuencia de la reactivación de un sistema de subducción longevo en el margen occidental de Sudamérica. A escala continental el Cretácico (90 Ma) y el Oligoceno (30 Ma) son considerados como importantes periodos de reorganización de la orogenia Andina. A nivel local los detalles del desarrollo de la orogenia varían dependiendo del segmento a considerar.
  • The Andean orogeny (Spanish: Orogenia andina) is an ongoing process of orogeny that began in the Early Jurassic and is responsible for the rise of the Andes mountains. The orogeny is driven by a reactivation of a long-lived subduction system along the western margin of South America. On a continental scale the Cretaceous (90 Ma) and Oligocene (30 Ma) were periods of re-arrangements in the orogeny. Locally the details of the nature of the orogeny varies depending on the segment and the geological period considered.
  • 安第斯造山運動（英語：Andean Orogeny）是一個在南美西岸的持續造山構造運動，始於侏羅紀早期，造成安第斯山脈上升的原因。在南美洲西部邊緣有一個長期存在的俯衝系統，經過重新激活這個俯衝系統，導致造山運動，在白堊紀（90 Ma）和漸新世（30 Ma）時期的造山運動，曾造成兩次造山帶重新排列。安第斯造山運動的地理位置很長，各地段均有其獨有的運動特徵和活動時期。
  • Андська складчастість (рос. андская (андийская) складчатость; англ. Andean folding; нім. andische Faltung f) — одна з епох мезозойської складчастості, яка виявилася в Андах Південної Америки.
  • Den andinska orogenesen är ett fortgående orogenes som verkat sedan Jura som lett till Andernas uphöjning. Orogenesen är ett resultat av omaktiveringen av ett långlivat subduktionssystem längs Sydamerikas västkust. I kontinental skala kan Krita (90 Ma) och Oligocen (30 Ma) utpekas som perioder av omorganisering i orogenesen. På lokal nivå så skiljer sig detaljerna av andinska orogenesen beroende på vilken segment och tidsintervall det handlar om.
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