The Anaximander Mountains: a clue to the tectonics of southwest Anatolia
| العنوان: | The Anaximander Mountains: a clue to the tectonics of southwest Anatolia |
|---|---|
| المؤلفون: | J.M. Woodside, Tiphaine A. C. Zitter, Jean Mascle |
| المساهمون: | Géoazur (GEOAZUR 6526), Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Université Nice Sophia Antipolis (... - 2019) (UNS), COMUE Université Côte d'Azur (2015-2019) (COMUE UCA)-COMUE Université Côte d'Azur (2015-2019) (COMUE UCA)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de la Côte d'Azur, Université Côte d'Azur (UCA)-COMUE Université Côte d'Azur (2015-2019) (COMUE UCA)-Université Côte d'Azur (UCA)-Centre National de la Recherche Scientifique (CNRS), Sedimentology, Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Université Nice Sophia Antipolis (1965 - 2019) (UNS), COMUE Université Côte d'Azur (2015-2019) (COMUE UCA)-Université Côte d'Azur (UCA)-Université Côte d'Azur (UCA)-Centre National de la Recherche Scientifique (CNRS) |
| المصدر: | Geological Journal Geological Journal, Wiley, 2003, 38 (3-4), pp.375-394. ⟨10.1002/gj.961⟩ Zitter, T A C, Woodside, J M & Mascle, J 2003, ' The Anaximander Mountains: a clue to the tectonics of southwest Anatolia ', Geological Journal, vol. 38, pp. 375-394 . https://doi.org/10.1002/gj.961 Geological Journal, 38, 375-394. John Wiley and Sons Ltd Geological Journal, 2003, 38 (3-4), pp.375-394. ⟨10.1002/gj.961⟩ |
| سنة النشر: | 2003 |
| مصطلحات موضوعية: | Rift, 010504 meteorology & atmospheric sciences, Transtension, Geology, Structural basin, 010502 geochemistry & geophysics, 01 natural sciences, Neotectonics, Paleontology, Tectonics, Eastern mediterranean, Submarine pipeline, SDG 14 - Life Below Water, Seismology, 0105 earth and related environmental sciences |
| الوصف: | The offshore Anaximander Mountains are an important link between the Hellenic and Cyprus arcs. They were formed by southeastward rifting from Turkey in post-Miocene time. Gravity data have shown that the eastern part of the Anaximander Mountains is different from the western part; multibeam mapping seems to confirm that the eastern Anaximander Mountains have affinity with the Florence Rise structure (western Cyprus Arc). Faulting along and across the latter feature is characterized in the seismic data by anastomosing faults and pop-up flower structures. It is likely that progressive adjustment to incipient collision developed into a broad zone of NW–SE transpressive wrenching extending towards south Turkey. In contrast, the western mountains are more directly related to the opening of the Rhodes Basin and the Finike Basin, as transtension may have dominated in southwest Turkey since the Pliocene. The connection with onshore Turkey is still unclear, but could be related to the Fethiye–Burdur Fault Zone that defines the western boundary of the complex Isparta Angle. The Anaximander Mountains and the Isparta Angle form together a tectonic accommodation zone between the active deformation in southwestern Turkey and the Aegean region and the tectonically quieter Cyprus region. Copyright # 2003 John Wiley & Sons, Ltd. |
| اللغة: | English |
| تدمد: | 0072-1050 1099-1034 |
| DOI: | 10.1002/gj.961⟩ |
| DOI: | 10.1002/gj.961 |
| URL الوصول: | https://explore.openaire.eu/search/publication?articleId=doi_dedup___::59cc51fe9a445151f6c0d922741f9c6d https://hdl.handle.net/1871.1/515ae51d-e5cc-49bc-baee-2df911647c61 |
| Rights: | RESTRICTED |
| رقم الانضمام: | edsair.doi.dedup.....59cc51fe9a445151f6c0d922741f9c6d |
| قاعدة البيانات: | OpenAIRE |
| تدمد: | 00721050 10991034 |
|---|---|
| DOI: | 10.1002/gj.961⟩ |