The Ayyubid Orogen: An Ophiolite Obduction-Driven Orogen in the Late Cretaceous of the Neo-Tethyan South Margin
A minimum 5000-km long obduction-driven orogeny of medial to late Cretaceous age is located between Cyrenaica in eastern Libya and Oman. It is herein called the Ayyubid Orogen after the Ayyubid Empire that covered much of its territory. The Ayyubid orogen is distinct from other Alpide orogens and ha...
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Geological Association of Canada
2014
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ftcaltechauth:oai:authors.library.caltech.edu:46258 2023-05-15T17:22:25+02:00 The Ayyubid Orogen: An Ophiolite Obduction-Driven Orogen in the Late Cretaceous of the Neo-Tethyan South Margin Şengör, A. M. Celâl Stock, Joann 2014 https://authors.library.caltech.edu/46258/ https://resolver.caltech.edu/CaltechAUTHORS:20140613-081909428 unknown Geological Association of Canada Şengör, A. M. Celâl and Stock, Joann (2014) The Ayyubid Orogen: An Ophiolite Obduction-Driven Orogen in the Late Cretaceous of the Neo-Tethyan South Margin. Geoscience Canada, 41 . pp. 225-254. ISSN 0315-0941. doi:10.12789/geocanj.2014.41.042. https://resolver.caltech.edu/CaltechAUTHORS:20140613-081909428 <https://resolver.caltech.edu/CaltechAUTHORS:20140613-081909428> Article PeerReviewed 2014 ftcaltechauth https://doi.org/10.12789/geocanj.2014.41.042 2021-11-11T18:58:07Z A minimum 5000-km long obduction-driven orogeny of medial to late Cretaceous age is located between Cyrenaica in eastern Libya and Oman. It is herein called the Ayyubid Orogen after the Ayyubid Empire that covered much of its territory. The Ayyubid orogen is distinct from other Alpide orogens and has two main parts: a western, mainly germanotype belt and an eastern mainly alpinotype belt. The germanotype belt formed largely as a result of an aborted obduction, whereas the alpinotype part formed as a result of successful and large-scale obduction events that choked a nascent subduction zone. The mainly germanotype part coincides with Erich Krenkel's Syrian Arc (Syrischer Bogen) and the alpinotype part with Ricou's Peri-Arabian Ophiolitic Crescent (Croissant Ophiolitique péri-Arabe). These belts formed as a consequence of the interaction of one of the now-vanished Tethyan plates and Afro-Arabia. The Africa-Eurasia relative motion has influenced the orogen's evolution, but was not the main causative agent. Similar large and complex obduction-driven orogens similar to the Ayyubids may exist along the Ordovician Newfoundland/Scotland margin of the Caledonides and along the Ordovician European margin of the Uralides. Article in Journal/Newspaper Newfoundland Caltech Authors (California Institute of Technology) Bogen ENVELOPE(13.109,13.109,66.324,66.324) Geoscience Canada 41 2 225 |
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Caltech Authors (California Institute of Technology) |
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unknown |
description |
A minimum 5000-km long obduction-driven orogeny of medial to late Cretaceous age is located between Cyrenaica in eastern Libya and Oman. It is herein called the Ayyubid Orogen after the Ayyubid Empire that covered much of its territory. The Ayyubid orogen is distinct from other Alpide orogens and has two main parts: a western, mainly germanotype belt and an eastern mainly alpinotype belt. The germanotype belt formed largely as a result of an aborted obduction, whereas the alpinotype part formed as a result of successful and large-scale obduction events that choked a nascent subduction zone. The mainly germanotype part coincides with Erich Krenkel's Syrian Arc (Syrischer Bogen) and the alpinotype part with Ricou's Peri-Arabian Ophiolitic Crescent (Croissant Ophiolitique péri-Arabe). These belts formed as a consequence of the interaction of one of the now-vanished Tethyan plates and Afro-Arabia. The Africa-Eurasia relative motion has influenced the orogen's evolution, but was not the main causative agent. Similar large and complex obduction-driven orogens similar to the Ayyubids may exist along the Ordovician Newfoundland/Scotland margin of the Caledonides and along the Ordovician European margin of the Uralides. |
format |
Article in Journal/Newspaper |
author |
Şengör, A. M. Celâl Stock, Joann |
spellingShingle |
Şengör, A. M. Celâl Stock, Joann The Ayyubid Orogen: An Ophiolite Obduction-Driven Orogen in the Late Cretaceous of the Neo-Tethyan South Margin |
author_facet |
Şengör, A. M. Celâl Stock, Joann |
author_sort |
Şengör, A. M. Celâl |
title |
The Ayyubid Orogen: An Ophiolite Obduction-Driven Orogen in the Late Cretaceous of the Neo-Tethyan South Margin |
title_short |
The Ayyubid Orogen: An Ophiolite Obduction-Driven Orogen in the Late Cretaceous of the Neo-Tethyan South Margin |
title_full |
The Ayyubid Orogen: An Ophiolite Obduction-Driven Orogen in the Late Cretaceous of the Neo-Tethyan South Margin |
title_fullStr |
The Ayyubid Orogen: An Ophiolite Obduction-Driven Orogen in the Late Cretaceous of the Neo-Tethyan South Margin |
title_full_unstemmed |
The Ayyubid Orogen: An Ophiolite Obduction-Driven Orogen in the Late Cretaceous of the Neo-Tethyan South Margin |
title_sort |
ayyubid orogen: an ophiolite obduction-driven orogen in the late cretaceous of the neo-tethyan south margin |
publisher |
Geological Association of Canada |
publishDate |
2014 |
url |
https://authors.library.caltech.edu/46258/ https://resolver.caltech.edu/CaltechAUTHORS:20140613-081909428 |
long_lat |
ENVELOPE(13.109,13.109,66.324,66.324) |
geographic |
Bogen |
geographic_facet |
Bogen |
genre |
Newfoundland |
genre_facet |
Newfoundland |
op_relation |
Şengör, A. M. Celâl and Stock, Joann (2014) The Ayyubid Orogen: An Ophiolite Obduction-Driven Orogen in the Late Cretaceous of the Neo-Tethyan South Margin. Geoscience Canada, 41 . pp. 225-254. ISSN 0315-0941. doi:10.12789/geocanj.2014.41.042. https://resolver.caltech.edu/CaltechAUTHORS:20140613-081909428 <https://resolver.caltech.edu/CaltechAUTHORS:20140613-081909428> |
op_doi |
https://doi.org/10.12789/geocanj.2014.41.042 |
container_title |
Geoscience Canada |
container_volume |
41 |
container_issue |
2 |
container_start_page |
225 |
_version_ |
1766109063382302720 |