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Acadian orogeny

 
Sci-Tech Dictionary: Acadian orogeny
(ə′kād·ē·ən ör′äj·ə·nē)

(geology) The period of formation accompanied by igneous intrusion that took place during the Middle and Late Devonian in the Appalachian Mountains.


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Britannica Concise Encyclopedia: Acadian orogeny
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Mountain-building event that affected the northern portion of the Appalachian Geosyncline from present-day New York to Newfoundland during the Devonian period. The orogeny was most intense in northern New England. Its origin has been ascribed to the collision of the northeastern portion of the North American Plate with western Europe. Evidence for the orogeny includes deformation of pre-Devonian and Devonian rocks.

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Wikipedia: Acadian orogeny
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The Acadian orogeny is a middle Paleozoic mountain building event (orogeny), especially in the northern Appalachians, between New York and Newfoundland. The Acadian orogeny most greatly affected the Northern Appalachian region (New England northeastward into the Gaspé region of Canada). The Acadian orogeny should not be regarded as a single tectonic event, but rather as an orogenic era. It spanned a period of about 50 million years, from 375 to 325 million years ago. 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. During the course of the orogeny, older rocks were deformed and metamorphosed, and new faults formed and older faults were reactivated.[1]

It was roughly 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.

Geodynamics

The cause of this great period of deformation is a result of the plate-docking of a small continental landmass called Avalonia (named after the Avalon Peninsula of Newfoundland). The docking of Avalonia onto the composite margin of Ganderia and Laurentia resulted in the closing of a portion of the Rheic Ocean. [2]

Avalonia was gradually torn apart as plate tectonic forces accreted the landmass onto the edge of the larger North American continent. Today, portions of the ancient Avalonia landmass occur in scattered outcrop belts along the eastern margin of North America. One belt occurs in Newfoundland, another forms the bedrock of much of the coastal region of New England from eastern Connecticut to northern Maine.[1]

A period of lithospheric thinning that followed the Acadian orogeny created volcanoes, such as the large Mount Pleasant Caldera in southwestern New Brunswick, Canada.

See also

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

 
 

 

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