دورية أكاديمية
Geology of the Central Sivas Basin (Turkey)
| العنوان: | Geology of the Central Sivas Basin (Turkey) |
|---|---|
| المؤلفون: | Legeay, Etienne, Pichat, Alexandre, Kergaravat, Charlie, Ribes, Charlotte, Callot, Jean-Paul, Ringenbach, Jean-Claude, Bonnel, Cedric, Hoareau, Guilhem, Poisson, Andre, Mohn, Geoffroy, Crumeyrolle, Phillipe, Kavak, Kaan Sevki, Temiz, Haluk |
| المساهمون: | Legeay, Etienne -- Pichat, Alexandre -- Kergaravat, Charlie -- Ribes, Charlotte -- Callot, Jean-Paul -- Bonnel, Cedric -- Hoareau, Guilhem Univ Pau & Pays Adour, Lab Fluides Complexes & Leurs Reservoirs, Pau, France -- Legeay, Etienne -- Pichat, Alexandre -- Kergaravat, Charlie -- Ribes, Charlotte -- Ringenbach, Jean-Claude -- Crumeyrolle, Phillipe CSTJF, Total SA, Pau, France -- Poisson, Andre Univ Paris XI Paris Sud, Sci Terre, Orsay, France -- Mohn, Geoffroy Univ Cergy Pontoise, Geosci Environm Cergy, Cergy Pontoise, France -- Kavak, Kaan Sevki -- Temiz, Haluk Cumhuriyet Univ, Dept Geol Engn, Sivas, Turkey, Mohn, Geoffroy -- 0000-0002-8729-2960, CALLOT, Jean-Paul -- 0000-0001-9385-3974 |
| بيانات النشر: | TAYLOR & FRANCIS LTD |
| سنة النشر: | 2019 |
| المجموعة: | Sivas Cumhuriyet University Institutional Repository |
| مصطلحات موضوعية: | Sivas Basin, salt-thrust-belt, salt tectonics, minibasins, Turkey, Anatolia |
| الوصف: | WOS: 000468176400001 ; This paper presents a revised geological map at the 1/50,000 scale of the Central Sivas Basin together with a synthetic stratigraphic chart and cross-sections. The map covers an area of approximately 9840 km (2) within the Eastern Anatolian orogen. The structure of the studied area is dominated by three major tectonic domains: (i) to the south, a north-verging thrust wedge involving Maastrichtian -Eocene sediments deposited onto an ophiolitic basement, (ii) in the center an Oligo-Miocene domain shaped by salt tectonics detached above the thrust wedge, along a late Eocene salt layer, and, (iii) to the north the Pliocene depocenter onlapping onto the Kirsehir basement. The central halokinetic domain exhibits two generations of minibasins (respectively, early Oligocene and late Oligocene to late Miocene), separated by an evaporite canopy. The map includes new stratigraphic correlations for the pre-salt stratigraphy and improve the comprehension of the southern fold-and-thrust-belt. ; Total S.A.; Pau Pays Adour ; This work has been made possible by funding from Total S.A. in the framework of the Structural Geology Chair at E2S-Univ. Pau & Pays Adour held by Jean-Paul Callot. |
| نوع الوثيقة: | article in journal/newspaper |
| اللغة: | English |
| تدمد: | 1744-5647 |
| العلاقة: | JOURNAL OF MAPS; Makale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı; https://dx.doi.org/10.1080/17445647.2018.1514539Test; https://hdl.handle.net/20.500.12418/5862Test; 15; 417; 406 |
| DOI: | 10.1080/17445647.2018.1514539 |
| الإتاحة: | https://doi.org/20.500.12418/5862Test https://doi.org/10.1080/17445647.2018.1514539Test https://hdl.handle.net/20.500.12418/5862Test |
| حقوق: | info:eu-repo/semantics/openAccess |
| رقم الانضمام: | edsbas.D7253E9B |
| قاعدة البيانات: | BASE |
| تدمد: | 17445647 |
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| DOI: | 10.1080/17445647.2018.1514539 |