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The Antler orogeny was a tectonic event that began in the early Late Devonian with widespread effects continuing into the Mississippian and early Pennsylvanian. Most of the evidence for this event is in Nevada but the limits of its reach are unknown. A great volume of conglomeratic deposits of mainly Mississippian age in Nevada and adjacent areas testifies to the existence of an important tectonic event, and implies nearby areas of uplift and erosion, but the nature and cause of that event are uncertain and in dispute. Although it is known as an orogeny (mountain building event), some of the classic features of orogeny as commonly defined such as metamorphism, and granitic intrusives have not been linked to it. In spite of this, the event is universally designated as an orogeny and that pr

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  • Antler orogeny (en)
  • Orogenesi Antler (it)
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  • The Antler orogeny was a tectonic event that began in the early Late Devonian with widespread effects continuing into the Mississippian and early Pennsylvanian. Most of the evidence for this event is in Nevada but the limits of its reach are unknown. A great volume of conglomeratic deposits of mainly Mississippian age in Nevada and adjacent areas testifies to the existence of an important tectonic event, and implies nearby areas of uplift and erosion, but the nature and cause of that event are uncertain and in dispute. Although it is known as an orogeny (mountain building event), some of the classic features of orogeny as commonly defined such as metamorphism, and granitic intrusives have not been linked to it. In spite of this, the event is universally designated as an orogeny and that pr (en)
  • L'orogenesi Antler è un evento tettonico che è iniziato nel Devoniano superiore, ma i cui effetti che sono poi proseguiti nel Mississippiano e fino all'inizio del Pennsylvaniano. Le maggiori evidenze di questo evento orogenetico si trovano nello Stato americano del Nevada, ma i limiti dell'estensione non sono stati ben identificati. Grandi volumi di conglomerati di prevalente origine del Mississippiano che si trovano nel Nevada e nelle aree adiacenti, testimoniano l'esistenza di un importante evento tettonico e implicano anche le vicine aree di sollevamento tettonico e di erosione, ma la natura e le cause dell'evento sono ancora incerte e oggetto di discussioni. (it)
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  • The Antler orogeny was a tectonic event that began in the early Late Devonian with widespread effects continuing into the Mississippian and early Pennsylvanian. Most of the evidence for this event is in Nevada but the limits of its reach are unknown. A great volume of conglomeratic deposits of mainly Mississippian age in Nevada and adjacent areas testifies to the existence of an important tectonic event, and implies nearby areas of uplift and erosion, but the nature and cause of that event are uncertain and in dispute. Although it is known as an orogeny (mountain building event), some of the classic features of orogeny as commonly defined such as metamorphism, and granitic intrusives have not been linked to it. In spite of this, the event is universally designated as an orogeny and that practice is continued here. This article outlines what is known and unknown about the Antler orogeny and describes three current theories regarding its nature and origin. (en)
  • L'orogenesi Antler è un evento tettonico che è iniziato nel Devoniano superiore, ma i cui effetti che sono poi proseguiti nel Mississippiano e fino all'inizio del Pennsylvaniano. Le maggiori evidenze di questo evento orogenetico si trovano nello Stato americano del Nevada, ma i limiti dell'estensione non sono stati ben identificati. Grandi volumi di conglomerati di prevalente origine del Mississippiano che si trovano nel Nevada e nelle aree adiacenti, testimoniano l'esistenza di un importante evento tettonico e implicano anche le vicine aree di sollevamento tettonico e di erosione, ma la natura e le cause dell'evento sono ancora incerte e oggetto di discussioni. Alcune delle classiche caratteristiche collegate ad un evento orogenetico, come il metamorfismo e le intrusioni granitiche, non sono ancora state collegate all'evento. (it)
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