Evolution of an early Eocene pull‐apart basin in the Central Pontides (Northern Turkey): New insights into the origin of the North Anatolian Shear Zone
Although the North Anatolian Shear Zone is one of the main lithospheric‐scale strike‐slip deformation zone in the world, playing a prominent role in the complex geodynamic interaction among the Eurasian, Anatolian and Arabian plates, the onset time of its activity remains highly controversial. Here,...
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| Veröffentlicht in: | Terra nova (Oxford, England) England), 2017-12, Vol.29 (6), p.392-400 |
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| creator | Ottria, Giuseppe Pandolfi, Luca Catanzariti, Rita Da Prato, Simone Ellero, Alessandro Frassi, Chiara Göncüoğlu, Mehmet Cemal Marroni, Michele Ruffini, Leonardo Sayit, Kaan |
| description | Although the North Anatolian Shear Zone is one of the main lithospheric‐scale strike‐slip deformation zone in the world, playing a prominent role in the complex geodynamic interaction among the Eurasian, Anatolian and Arabian plates, the onset time of its activity remains highly controversial. Here, we tackle this issue by utilizing nannofossil biostratigraphy on deposits from the Taşcilar basin, a pull‐apart basin that we have identified inside the North Anatolian Shear Zone overprinting the Intra‐Pontide suture zone. The syn‐tectonic sedimentary succession of the Taşcilar basin developed completely during the early Eocene (Ypresian; CNE4–CNE5 Zones). The strike‐slip faulting related to the initial onset of the North Anatolian Shear Zone can likely be constrained within the Ypresian, suggesting that the westward escape of the Anatolian plate along the North Anatolian Shear Zone started in the early Eocene. |
| doi_str_mv | 10.1111/ter.12299 |
| format | Article |
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Here, we tackle this issue by utilizing nannofossil biostratigraphy on deposits from the Taşcilar basin, a pull‐apart basin that we have identified inside the North Anatolian Shear Zone overprinting the Intra‐Pontide suture zone. The syn‐tectonic sedimentary succession of the Taşcilar basin developed completely during the early Eocene (Ypresian; CNE4–CNE5 Zones). The strike‐slip faulting related to the initial onset of the North Anatolian Shear Zone can likely be constrained within the Ypresian, suggesting that the westward escape of the Anatolian plate along the North Anatolian Shear Zone started in the early Eocene.</description><identifier>ISSN: 0954-4879</identifier><identifier>EISSN: 1365-3121</identifier><identifier>DOI: 10.1111/ter.12299</identifier><language>eng</language><publisher>Oxford: Blackwell Publishing Ltd</publisher><subject>Basins ; Biostratigraphy ; Deformation ; Ecological succession ; Eocene ; Plates ; Shear zone ; Strike-slip faults</subject><ispartof>Terra nova (Oxford, England), 2017-12, Vol.29 (6), p.392-400</ispartof><rights>2017 John Wiley & Sons Ltd</rights><rights>Copyright © 2017 John Wiley & Sons Ltd</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a3209-a88c70067582f9da32ddd6f6c3a5370609a8a35f47211ed02f40ba2c8108f2f93</citedby><cites>FETCH-LOGICAL-a3209-a88c70067582f9da32ddd6f6c3a5370609a8a35f47211ed02f40ba2c8108f2f93</cites><orcidid>0000-0002-0797-5500 ; 0000-0002-4360-0466 ; 0000-0002-4216-6995 ; 0000-0002-0221-8623 ; 0000-0001-6859-4536 ; 0000-0002-6408-0543 ; 0000-0002-2947-3739 ; 0000-0002-6129-647X ; 0000-0002-7522-9905</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1111%2Fter.12299$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1111%2Fter.12299$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,776,780,1411,27903,27904,45553,45554</link.rule.ids></links><search><creatorcontrib>Ottria, Giuseppe</creatorcontrib><creatorcontrib>Pandolfi, Luca</creatorcontrib><creatorcontrib>Catanzariti, Rita</creatorcontrib><creatorcontrib>Da Prato, Simone</creatorcontrib><creatorcontrib>Ellero, Alessandro</creatorcontrib><creatorcontrib>Frassi, Chiara</creatorcontrib><creatorcontrib>Göncüoğlu, Mehmet Cemal</creatorcontrib><creatorcontrib>Marroni, Michele</creatorcontrib><creatorcontrib>Ruffini, Leonardo</creatorcontrib><creatorcontrib>Sayit, Kaan</creatorcontrib><title>Evolution of an early Eocene pull‐apart basin in the Central Pontides (Northern Turkey): New insights into the origin of the North Anatolian Shear Zone</title><title>Terra nova (Oxford, England)</title><description>Although the North Anatolian Shear Zone is one of the main lithospheric‐scale strike‐slip deformation zone in the world, playing a prominent role in the complex geodynamic interaction among the Eurasian, Anatolian and Arabian plates, the onset time of its activity remains highly controversial. 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| ispartof | Terra nova (Oxford, England), 2017-12, Vol.29 (6), p.392-400 |
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| language | eng |
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| source | Wiley Online Library All Journals |
| subjects | Basins Biostratigraphy Deformation Ecological succession Eocene Plates Shear zone Strike-slip faults |
| title | Evolution of an early Eocene pull‐apart basin in the Central Pontides (Northern Turkey): New insights into the origin of the North Anatolian Shear Zone |
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