Log InRegister
Quick Links : The Mindat ManualThe Rock H. Currier Digital LibraryMindat Newsletter [Free Download]
Home PageAbout MindatThe Mindat ManualHistory of MindatCopyright StatusWho We AreContact UsAdvertise on Mindat
Donate to MindatCorporate SponsorshipSponsor a PageSponsored PagesMindat AdvertisersAdvertise on Mindat
Learning CenterWhat is a mineral?The most common minerals on earthInformation for EducatorsMindat ArticlesThe ElementsThe Rock H. Currier Digital LibraryGeologic Time
Minerals by PropertiesMinerals by ChemistryAdvanced Locality SearchRandom MineralRandom LocalitySearch by minIDLocalities Near MeSearch ArticlesSearch GlossaryMore Search Options
Search For:
Mineral Name:
Locality Name:
Keyword(s):
 
The Mindat ManualAdd a New PhotoRate PhotosLocality Edit ReportCoordinate Completion ReportAdd Glossary Item
Mining CompaniesStatisticsUsersMineral MuseumsClubs & OrganizationsMineral Shows & EventsThe Mindat DirectoryDevice SettingsThe Mineral Quiz
Photo SearchPhoto GalleriesSearch by ColorNew Photos TodayNew Photos YesterdayMembers' Photo GalleriesPast Photo of the Day GalleryPhotography

Brun, Jean-Pierre, Faccenna, Claudio, Gueydan, Frédéric, Sokoutis, Dimitrios, Philippon, Mélody, Kydonakis, Konstantinos, Gorini, Christian (2016) The two-stage Aegean extension, from localized to distributed, a result of slab rollback acceleration. Canadian Journal of Earth Sciences, 53 (11) 1142-1157 doi:10.1139/cjes-2015-0203

Advanced
   -   Only viewable:
Reference TypeJournal (article/letter/editorial)
TitleThe two-stage Aegean extension, from localized to distributed, a result of slab rollback acceleration
JournalCanadian Journal of Earth Sciences
AuthorsBrun, Jean-PierreAuthor
Faccenna, ClaudioAuthor
Gueydan, FrédéricAuthor
Sokoutis, DimitriosAuthor
Philippon, MélodyAuthor
Kydonakis, KonstantinosAuthor
Gorini, ChristianAuthor
Year2016 (November)Volume53
Page(s)1142-1157Issue11
PublisherCanadian Science Publishing
DOIdoi:10.1139/cjes-2015-0203Search in ResearchGate
Mindat Ref. ID485195Long-form Identifiermindat:1:5:485195:4
GUID66563f92-aeff-459a-9fbd-866cbf7faadc
Full ReferenceBrun, Jean-Pierre, Faccenna, Claudio, Gueydan, Frédéric, Sokoutis, Dimitrios, Philippon, Mélody, Kydonakis, Konstantinos, Gorini, Christian (2016) The two-stage Aegean extension, from localized to distributed, a result of slab rollback acceleration. Canadian Journal of Earth Sciences, 53 (11) 1142-1157 doi:10.1139/cjes-2015-0203
Plain TextBrun, Jean-Pierre, Faccenna, Claudio, Gueydan, Frédéric, Sokoutis, Dimitrios, Philippon, Mélody, Kydonakis, Konstantinos, Gorini, Christian (2016) The two-stage Aegean extension, from localized to distributed, a result of slab rollback acceleration. Canadian Journal of Earth Sciences, 53 (11) 1142-1157 doi:10.1139/cjes-2015-0203
In(2016, November) Canadian Journal of Earth Sciences Vol. 53 (11) Canadian Science Publishing
Abstract/Notes Back-arc extension in the Aegean, which was driven by slab rollback since 45 Ma, is described here for the first time in two stages. From Middle Eocene to Middle Miocene, deformation was localized leading to (i) the exhumation of high-pressure metamorphic rocks to crustal depths, (ii) the exhumation of high-temperature metamorphic rocks in core complexes, and (iii) the deposition of sedimentary basins. Since Middle Miocene, extension distributed over the whole Aegean domain controlled the deposition of onshore and offshore Neogene sedimentary basins. We reconstructed this two-stage evolution in 3D and four steps at Aegean scale by using available ages of metamorphic and sedimentary processes, geometry, and kinematics of ductile deformation, paleomagnetic data, and available tomographic models. The restoration model shows that the rate of trench retreat was around 0.6 cm/year during the first 30 My and then accelerated up to 3.2 cm/year during the last 15 My. The sharp transition observed in the mode of extension, localized versus distributed, in Middle Miocene correlates with the acceleration of trench retreat and is likely a consequence of the Hellenic slab tearing documented by mantle tomography. The development of large dextral northeast–southwest strike-slip faults, since Middle Miocene, is illustrated by the 450 km long fault zone, offshore from Myrthes to Ikaria and onshore from Izmir to Balikeshir, in Western Anatolia. Therefore, the interaction between the Hellenic trench retreat and the westward displacement of Anatolia started in Middle Miocene, almost 10 Ma before the propagation of the North Anatolian Fault in the North Aegean.

References Listed

These are the references the publisher has listed as being connected to the article. Please check the article itself for the full list of references which may differ. Not all references are currently linkable within the Digital Library.

Bargnesi, E.A., Stockli, D.F., Mancktelow, N.N., and Soukis, K. 2013. Miocene core complex development and coeval supradetachment basin evolution of Paros, Greece, insights from (U–Th)/He thermochronometry. Tectonophysics, 595–596: 165–182. 10.1016/j.tecto.2012.07.015.
Burg, J.P. 2012. Rhodope: From Mesozoic convergence to Cenozoic extension. Review of petro-structural data in the geochronological frame. In The Geology of Greece. Edited by E. Skourtsos and G.S. Lister. Journal of the Virtual Explorer, Vol. 42.
Not Yet Imported: Facies - journal-article : 10.1007/BF02537362

If you would like this item imported into the Digital Library, please contact us quoting Journal ID 23070
()
Christodoulou G. (1965) Bulletin of the Geological Society of Greece , 249
()
Dimitriadis S. (1989) Geologica Rhodopica 1, 190
()
Not Yet Imported: Active Continental Margins — Present and Past - book-chapter : 10.1007/978-3-662-38521-0_5

If you would like this item imported into the Digital Library, please contact us quoting Book ID 9783662377093
Gautier P. (1990) Comptes Rendus de l’Académie des Sciences, Paris 310, 147
Jones, K.D. 1971. An outline of the geology of the islands of Mytilini and Chios. In Geology and history of Turkey. Edited by A.S. Campbell. Petroleum Exploration Society of Libya, Tripoli. pp. 275–282.
Kolocotroni C. (1991) Bulletin of the Geological Society of Greece 25, 469
Koufos G.D. (2009) Biochronology. Beiträge zur Paläontologie 31, 397
Lalechos N. (1986) Lithos 56, 89
Lyberis, N. 1984. Tectonic evolution of the North Aegean Trough. Geological Society, London, Special Publications, Vol. 17, pp. 709–725. 10.1144/GSL.SP.1984.017.01.57.
Mercier J.-L. (1987) Annales Tectonicae 1, 20
Not Yet Imported: Postcollisional Tectonics and Magmatism in the Mediterranean Region and Asia - book-chapter : 10.1130/2006.2409(11)

If you would like this item imported into the Digital Library, please contact us quoting Journal ID
Not Yet Imported: Journal of the Virtual Explorer - journal-article : 10.3809/jvirtex.2007.00180

If you would like this item imported into the Digital Library, please contact us quoting Journal ID 48610
Not Yet Imported: Journal of the Virtual Explorer - journal-article : 10.3809/jvirtex.2007.00181

If you would like this item imported into the Digital Library, please contact us quoting Journal ID 48610
Salaün, G. 2011. Structure et déformation du manteau supérieur de la région Egée-Anatolie par tomographie en ondes de Rayleigh. PhD thesis, University of Grenoble.
Urai, V.L., Shuiling, R.D., and Jansen, J.B.H. 1990. Alpine deformation on Naxos (Greece). In Deformation Mechanisms. Edited by R.J. Knipe and E.H. Rutter. Rheology and Tectonics Geological Society, Special Publications, Vol. 54, pp. 509–522.
Widiyantoro S. (2004) International Journal of Tomography and Statistics 04, 1
Wuthrich, E. 2009. Low temperature thermochronology of the North Aegean Rhodope Massif. Ph.D. thesis, Swiss Federal Institute of Technology, Zurich.


See Also

These are possibly similar items as determined by title/reference text matching only.

 
and/or  
Mindat Discussions Facebook Logo Instagram Logo Discord Logo
Mindat.org is an outreach project of the Hudson Institute of Mineralogy, a 501(c)(3) not-for-profit organization.
Copyright © mindat.org and the Hudson Institute of Mineralogy 1993-2024, except where stated. Most political location boundaries are © OpenStreetMap contributors. Mindat.org relies on the contributions of thousands of members and supporters. Founded in 2000 by Jolyon Ralph.
Privacy Policy - Terms & Conditions - Contact Us / DMCA issues - Report a bug/vulnerability Current server date and time: May 10, 2024 11:40:11
Go to top of page