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Paleozoic evolution of the Armorica Plate on the basis of paleomagnetic data
New data support the contention that Armorica and Gondwana formed a coherent block until Ordovician time. However, by Early Devonian time, Armorica collided with the North American-northern European assembly to form the Old Red Continent, and the collision itself was responsible for the Acadian Orog...
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Published in: | Geology (Boulder) 1984-10, Vol.12 (10), p.579-582 |
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container_end_page | 582 |
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container_start_page | 579 |
container_title | Geology (Boulder) |
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creator | Perroud, Hervé Van der Voo, Rob Bonhommet, Norbert |
description | New data support the contention that Armorica and Gondwana formed a coherent block until Ordovician time. However, by Early Devonian time, Armorica collided with the North American-northern European assembly to form the Old Red Continent, and the collision itself was responsible for the Acadian Orogeny, not for the earlier Taconic Orogeny as postulated previously. The Carboniferous collision of Gondwana with the Old Red Continent subsequently formed Pangaea and produced the Appalachian-Hercynian Orogeny.—Modified journal abstract. |
doi_str_mv | 10.1130/0091-7613(1984)12<579:PEOTAP>2.0.CO;2 |
format | article |
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However, by Early Devonian time, Armorica collided with the North American-northern European assembly to form the Old Red Continent, and the collision itself was responsible for the Acadian Orogeny, not for the earlier Taconic Orogeny as postulated previously. The Carboniferous collision of Gondwana with the Old Red Continent subsequently formed Pangaea and produced the Appalachian-Hercynian Orogeny.—Modified journal abstract.</description><identifier>ISSN: 0091-7613</identifier><identifier>EISSN: 1943-2682</identifier><identifier>DOI: 10.1130/0091-7613(1984)12<579:PEOTAP>2.0.CO;2</identifier><language>eng</language><publisher>Geological Society of America (GSA)</publisher><subject>Acadian Phase ; Appalachian Phase ; Appalachians ; Armorica Plate ; Armorican Massif ; Atlantic region ; continental drift ; Devonian ; Europe ; evolution ; France ; Geophysics ; Gondwana ; mechanism ; North America ; Old Red Continent ; orogeny ; paleogeography ; paleomagnetism ; Paleozoic ; Pangaea ; Permian ; plate collision ; plate tectonics ; plates ; reconstruction ; solid Earth (tectonophysics) ; stratigraphy ; tectonophysics ; Variscan Orogeny ; Western Europe</subject><ispartof>Geology (Boulder), 1984-10, Vol.12 (10), p.579-582</ispartof><rights>GeoRef, Copyright 2020, American Geosciences Institute.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://pubs.geoscienceworld.org/lithosphere/article-lookup?doi=10.1130/0091-7613(1984)12<579:PEOTAP>2.0.CO;2$$EHTML$$P50$$Ggeoscienceworld$$H</linktohtml><link.rule.ids>314,780,784,27924,27925,38881,77824</link.rule.ids></links><search><creatorcontrib>Perroud, Hervé</creatorcontrib><creatorcontrib>Van der Voo, Rob</creatorcontrib><creatorcontrib>Bonhommet, Norbert</creatorcontrib><title>Paleozoic evolution of the Armorica Plate on the basis of paleomagnetic data</title><title>Geology (Boulder)</title><description>New data support the contention that Armorica and Gondwana formed a coherent block until Ordovician time. However, by Early Devonian time, Armorica collided with the North American-northern European assembly to form the Old Red Continent, and the collision itself was responsible for the Acadian Orogeny, not for the earlier Taconic Orogeny as postulated previously. 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issn | 0091-7613 1943-2682 |
language | eng |
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source | GeoScienceWorld |
subjects | Acadian Phase Appalachian Phase Appalachians Armorica Plate Armorican Massif Atlantic region continental drift Devonian Europe evolution France Geophysics Gondwana mechanism North America Old Red Continent orogeny paleogeography paleomagnetism Paleozoic Pangaea Permian plate collision plate tectonics plates reconstruction solid Earth (tectonophysics) stratigraphy tectonophysics Variscan Orogeny Western Europe |
title | Paleozoic evolution of the Armorica Plate on the basis of paleomagnetic data |
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