The Acadian orogeny is a middle Paleozoic deformation, especially in the northern Appalachians, between New York and Newfoundland. In Gaspé and adjacent areas, its climax is dated as early in the Late Devonian, but deformational, plutonic, and metamorphic events extended into Early Mississippian time. The Acadian should be regarded, not as a single orogenic episode, but rather as an orogenic era.

It appears to have been contemporaneous with the Bretonic phase of the Variscan orogeny of Europe, with metamorphic events in southwestern Texas and northern Mexico, and with the Antler orogeny of the Great Basin.

See also

• Iapetus Ocean
• Taconic orogeny

References

• Dictionary of Geological Terms, 3rd. Edition,1984, Robert L. Bates and Julia A. Jackson, Eds., prepared by The American Geological Institute
• International Tectonic Dictionary, 1967, Memoir 7, Am. Assoc. Petroleum Geologists, p. 114

Paleozoic | Plate tectonics | Geology of the United States

阿卡迪亞造山運動 | Akadische Orogenese