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  • image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    Authors: Kazanci, N.; Karadenizli, L.; Seyitoǧlu, G.; Sen, S.; +4 Authors

    The Akkaşdaǧι area, situated in the southern margin of the Tertiary Çankιrι-Çorum Basin, Central Anatolia, Turkey, includes a 280 m thick, mostly continental sediment sequence that overlies either marine Palaeogene transgressive deposits or metamorphic rocks of Kirşehir Massif. From bottom to top the sequence can be divided into units of Deliceirmak Fm. (alluvial fan deposits) and Ceritkale member (marine fan-delta and shelf carbonates) of mid-upper Eocene, Güvendik Fm. (gypsum) of Oligocene, and Akkaşdaǧι Fm. (fine to coarse-grained alluvial clastics and lacustrine limestone) of upper Miocene-lower Pliocene. A granitic intrusion was emplaced into the basin after late Eocene. The Neogene succession includes mammalian fossils and the lithological composition of the succession is rather different from its equivalences in other parts of the basin. By facies analysis die Neogene infill could be categorised into alluvial fan deposits (facies association I), fluvial deposits (facies association II), lacustrine deposits (facies association III) and pyroclastic flow deposits (facies association IV). Facies association I is dominant and the others are observed inside as alternating sequences. The facies architecture and facies associations suggest that a structural depression existed in the area and was filled with sediments of distal alluvial fans, flood plains and lakes receiving deposits of distal or terminal alluvial fans and flood plains, and occupied partly by lakes. © Publications Scientifiques du Muséum national d'Histoire naturelle, Paris.

    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/ ZENODOarrow_drop_down
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    Article . 2005
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    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
    ZENODO
    Article . 2005
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      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/ ZENODOarrow_drop_down
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      image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
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    Authors: Özpınar, Yahya; Hançer, Mete; Semiz, Barış;

    In this region, marine, continental and lacustrine clay deposits which are used as a raw material in the cement sector were investigated. It is seen that Upper Cretaceous-Upper Eocene shales representing marine deposition are found in Malidagi in economic quantities, However, their Na(2)O% and K(2)O% contents are higher than in other clays. The Oligocene aged Bayiralan clay representing marine deposition have abundant magnesian minerals. Because of its high MgO% content, this clay is not suitable cement standard. The areal extent of the Upper Miocene-Lower Pliocene Kizilburun clays represented fine sediments in the floodplain are widely situated. These may be used in cement sector, but the have reserve and environmental problems. The red coloured clays belonging to the Pliocene Sakizcilar Formation are sutitable for cement standard. To decreasing the transportation costs of the Denizli cement factory, the Malidagi clay and Sakizcilar clay may be used together in different proportions, If the Malidagi and Sakizcilar clays may be used, the contents of K(2)O% and Na(2)O% will decrease.

    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/ Pamukkale Üniversite...arrow_drop_down
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      image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
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  • image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
    Authors: Wesselingh, F.P.; Alçiçek, Hülya;

    Abstract: We present the first record of the cardiid genus Monodacna from the Pliocene of Anatolia, Turkey. Monodacna imrei sp. nov. was found in the Pliocene Killik Formation from the western margin of the Baklan Basin, in very marginal brackish to freshwater lacustrine deposits. The new record extends the stratigraphic range of the modern Ponto-Caspian genus back into the Pliocene and adds to earlier evidence that modern Ponto-Caspian taxa originated in the Pliocene of south-western Turkey. © The Palaeontological Association.

    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Pamukkale Üniversite...arrow_drop_down
    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
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      image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Pamukkale Üniversite...arrow_drop_down
      image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
  • image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
    Authors: Billi, A.; Berardi, G.; Gratier, J.-P.; Rossetti, F.; +7 Authors

    In our previous paper (Billi et al., 2017), using field geological observations, U-Th dating, and stable isotope analyses, we studied two deposits of Pleistocene thermogene travertines from Tuscany in central Italy. We concluded our study (1) warning that the common stratigraphic concept of travertine being a sedimentary succession with age younging from bottom to top is not always correct, (2) demonstrating that CaCO3 mineralization and veins can develop within the travertines after their formation with this syn-diagenetic process being able to modify the continuous bottom-up age evolution, and (3) showing that this post-depositional mineralization-veining process can not only modify the temporal succession but also deform and change the initial depositional travertine structure and its petrophysical properties. These conclusions could potentially make the interpretation of a travertine series more difficult than commonly thought. Alcicek et alii questioned our conclusions claiming that the travertine structures that we observed in Tuscany and interpreted as post-depositional features should have been interpreted, in analogy to similar structures from travertines elsewhere, as primary structures. Although we recognize, as already thoroughly stated in Billi et al. (2017), that the travertine depositional/post-depositional processes generally require further studies, we reaffirm the validity of our original interpretation at least for the structures analyzed in our previous paper. We, therefore, counter all criticisms by Alcicek et alii and conclude by indicating the way forward to further explore the depositional and post-depositional processes of thermogene travertines. © 2017 Elsevier B.V.

    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Pamukkale Üniversite...arrow_drop_down
    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
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      image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Pamukkale Üniversite...arrow_drop_down
      image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
  • image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    Authors: Alcicek, Mehmet Cihat; Mayda, Serdar; Titov, Vadim V.;

    The Burdur Basin is one of the NE-trending extensional orogen-top basins of SW Anatolia hosting alluvial-fan, fluvial and lacustrine deposits from the Late Miocene onward. The remains of Equus (Allohippus) sp., Paracamelus cf. gigas, and medium-sized deer (Cervidae gen. indet.) from the uppermost reach of the basin-fill succession show an interregional palaeobiogeographical linkage. The composition of fossil associations is typical for the wVillafranchian of eastern Europe and central Asia. The architecture of the basin-fill stratigraphy and associated fossil taxa refines the Early Pleistocene regional palaeogeography and biodiversity of Anatolia drawn over the Eurasian migration pattern. (C) 2012 Academie des sciences. Published by Elsevier Masson SAS. All rights reserved. The study was supported by international bilateral cooperation between The Scientific and Technological Research Council of Turkey and the Russian Foundation for Basic Research (TUBITAK-RFBR 111Y192 grant). MCA thanks the Turkish Academy of Sciences given the Outstanding Young Scientist Award, SM thanks the Ege University projects TTM/001/2010, TTM/002/2011 and VVT thanks the RFBR projects 12-05-91372-ST-a, 12-04-01691-a. Comments by Andrea Brogi and one anonymous reviewer are much appreciated. We wish to thank T.Tanju Kaya (Ege Univ.) and Hulya Alcicek (Pamukkale Univ.) for field help. Scientific and Technological Research Council of TurkeyTurkiye Bilimsel ve Teknolojik Arastirma Kurumu (TUBITAK); Russian Foundation for Basic ResearchRussian Foundation for Basic Research (RFBR) [TUBITAK-RFBR 111Y192]; Turkish Academy of SciencesTurkish Academy of Sciences; Ege UniversityEge University [TTM/001/2010, TTM/002/2011]; RFBRRussian Foundation for Basic Research (RFBR) [12-05-91372-ST-a, 12-04-01691-a] WOS: 000315702600001

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    Aperta - TÜBİTAK Açık Arşivi
    Other literature type . 2013
    License: CC BY
    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
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      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/ Pamukkale Üniversite...arrow_drop_down
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      Aperta - TÜBİTAK Açık Arşivi
      Other literature type . 2013
      License: CC BY
      image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
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  • image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
    Authors: Mehmet Cihat Alçiçek; Nizamettin Kazanci; Mehmet Özkul;

    The neotectonic development of western Anatolia was characterized by the formation of numerous graben-type basins, which have been well documented by general mapping, although the cause and timing of the Neogene regional tectonic extension remain controversial. Previous interpretations of the origin and evolution of these Neogene basins were based mainly on regional-scale tectonic inferences, rather than detailed basin-fill analysis. The present study of the terrestrial intramontane Çameli Basin in the western Taurides combines detailed facies analysis with biostratigraphic dating (mammalian and molluscan fossils) and documents three pulses of crustal extension that are reflected in changes in the palaeogeography and sedimentary architecture of the basin. Development of the Çameli graben commenced in the Vallesian time (early Tortonian), and is marked by alluvial-fan, fluvial and lacustrine depositional systems, with freshwater molluscan fauna. A second pulse of tectonic extension occurred in the late Ruscinian time (early-middle Pliocene), producing a new normal fault that split the basin longitudinally into two compartments. The lake environment expanded and deepened, coastal peat-forming mires developed and abundant mammal fauna appeared by the early Villanian time (middle Pliocene), with the lacustrine deposits onlapping the basin-margin and intrabasinal fault escarpments. The lacustrine environment subsequently shrank, as the progradation of axial river deltas and basin-margin fan deltas caused water shallowing and shoreline regression. A third pulse of extension occurred at the end of Villanian time (late Pliocene), when the development of a new generation of normal faults further split the basin into still narrower half-graben compartments. The third pulse of rifting is estimated to have accounted for little more than 10% of the sub-basinal crustal extension, but caused the most striking changes in the basin palaeogeography and drainage pattern. The inward development of the successive normal faults indicated a high-rate crustal extension. This is the first regional case study of a terrestrial neotectonic graben employing detailed sedimentary facies analysis and mammal biostratigraphy and providing a time-stratigraphic framework for the rifting pulses in western Anatolia. © 2004 Elsevier B.V. All rights reserved.

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    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
    Sedimentary Geology
    Article . 2005 . Peer-reviewed
    License: Elsevier TDM
    Data sources: Crossref
    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
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      image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Pamukkale GCRIS Data...arrow_drop_down
      image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
      image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
      Sedimentary Geology
      Article . 2005 . Peer-reviewed
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    Authors: Alçiçek, Mehmet Cihat.;

    The Eşen Basin of southwestern Anatolia formed as a NE-trending intramontane extensional graben, ca. 15 km wide and 30 km long, in the Early Tortonian, after the southeasterly emplacement of the Lycian nappes during the Tauride orogeny. The basin originated due to gravitational collapse of the hinterland zone of the Lycian Taurides in response to the lithospheric thickening caused by microcontinent collision. Sedimentation commenced with the development of basin-margin alluvial fans and a southward-directed axial fluvial system, the latter expanding laterally, changing its channel pattern from braided to meandering and forming floodplain lakes. The isolated ephemeral lakes merged into a single lake at the basin centre, fringed with vegetated mires and desiccated by the end of Miocene time. The second pulse of rifting in the basin, dated to the Early Pliocene, is attributed to the roll-back and outward expansion of the Cretan subduction arc to the south. A new lake rapidly expanded, and the Pliocene deposition of a thick marly succession was terminated by the basinward advance of Gilbert-type deltas and gradual desiccation of the lake in the Late Pliocene. The third pulse of rifting, near the end of the Pliocene, formed new faults, tilted the basin-fill succession and records regional deformation due to the westward tectonic expulsion of the Anatolian craton. The base of the overlying Pleistocene alluvium is an angular unconformity, with fluvial terraces indicating considerable Quaternary uplift. The developmental stages of the Eşen Basin are consistent with the tectonostatigraphic evolution of the adjacent Çameli Basin to the north, which may thus serve as a reference framework for the tectonic history of the region's extensional grabens. © 2007 Elsevier B.V. All rights reserved.

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    Sedimentary Geology
    Article . 2007 . Peer-reviewed
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      Sedimentary Geology
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    Authors: Wesselingh, F.P.; Alçiçek, Hülya; Magyar, I.;

    We report on a Late Miocene mollusc fauna from a single locality in the Denizli Basin in Southwestern Turkey that is composed of ten presumably euryhaline species and three freshwater species. The fauna is remarkably distinct from faunas of the adjacent Late Miocene Aegean and Euxinian Basins, and has elements in common with the modern Caspian Sea fauna in the form of Didacna species. The Suggested age of the fauna (Late Miocene) would extend the stratigraphic range of the lymnocardiid genus Didacna (hitherto Calabrian-Extant) considerably. The palaeobiogeographic significance of the Denizli fauna is discussed. (C) 2008 Elsevier Masson SAS. All rights reserved.

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    Geobios; Pamukkale GCRIS Database
    Article . 2008 . Peer-reviewed
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      Geobios; Pamukkale GCRIS Database
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    Authors: Ezher Toker; Mine Sezgül Kayseri-Özer; Mehmet Özkul; Sándor Kele;

    AbstractTravertine deposits in western Turkey are very well‐exposed in the area of Kocabaş, in the eastern part of the Denizli Basin. The palaeoclimatic significance of these travertines is discussed using U/Th dates, stable isotope data and palynological evidence. The Kocabaş travertine occurrences are characterized by successions of depositional terraces associated with palaeosols and karstic features. The travertines have been classified into eight lithotypes and one erosional horizon, namely: laminated, coated bubble, reed, paper‐thin raft, intraclasts, micritic travertine with gastropods, extra‐formational pebbles and a palaeosol layer. The analysed travertines mostly formed between 181 ka and 80 ka (Middle to Late Pleistocene) during a series of climatic changes including glacial and interglacial intervals; their δ13C and δ18O values indicate that the depositional waters were mainly of basinal thermal origin, occasionally mixed with surficial meteoric water. Palynological results obtained from the palaeosols showed an abundance of non‐arboreal percentage and xerophytic plants (Oleaceae and Quercus evergreen type) indicating that a drought occurred. Marine Isotope Stage 6 is represented by grassland species but Marine Isotope Stage 5 is represented by Pinaceae–Pinus and Abies, Quercus and Oleaceae. Uranium/thorium analyses of the Kocabaş travertines show that deposition began in Marine Isotope Stage 6 (glacial) and continued to Marine Isotope Stage 4 (glacial), but mostly occurred in Marine Isotope Stage 5 (interglacial). The travertine deposition continued to ca 80 ka in the south‐west of the study area, in one particular depression depositional system. Palaeoenvironmental indicators suggest that the travertine depositional evolution was probably controlled by fault‐related movements that influenced groundwater flow. Good correlation of the stable isotope values and dates of deposition of the travertines and palynological data of palaeosols in the Kocabaş travertines serve as a starting point for further palaeoclimate studies in south‐west Turkey. Additionally, the study can be compared with other regional palaeoclimate archives.

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    Sedimentology
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    Authors: Kaya, Ali;

    Doğu Toroslar’da yer alan Keban Metamorfitleri, yeşilşist fasiyesinde bölgesel metamorfizmaya uğramış platform tipi karbonat ve kırıntılı kayaçlardan oluşur. Keban metamorfitlerinin yaşı, Zeryanderedeki tek bir lokasyonda gözlenen ve Permiyen yaşlı olduğu tahmin edilen, türleri saptanamamış mikroorganizmalara ait iki fosil (Glomospira ve Ammodiscus familyasına ait fosiller) bulgusuna dayandırılmıştır. Metamorfik istifteki diğer formasyonlar da bu seviyeyle korele edilerek, Keban metamorfitleri için Permo-Triyas/Permo-Karbonifer yaşları önerilmiş ve şimdiye kadar kullanılmıştır. Bölgenin bütün jeolojik değerlendirmeleri de bu yaşlara göre yapılmıştır. İlk defa bu çalışmada, çok yaygın bir şekilde Planolites, Rhizocorallium ve Thalassinoides gibi iz fosiller gözlenmiştir. Bu iz fosiller, Keban metamorfitlerinin orta seviyelerini temsil eden Nimri formasyonuna ait Gogodere tabakalı dolomitik-kristalize kireçtaşı üyesinin tabaka üst yüzeylerinde tespit edilmiştir. Bu iz fosilleri içeren kireçtaşı seviyeleri, Toroslar’da Erken-Orta Triyas’ı (Skitiyen-Anisiyen) temsil eden tipik “vermiküler kireçtaşı fasiyesi”ne karşılık gelmektedir. Allokton konumlu Keban metamorfitleri, birbirlerini üzerleyen birkaç naptan oluşmaktadır. Çalışma alanı içinde üç nap vardır; en alt napı Erken Triyas-Jura yaşlı Nimri formasyonu oluşturur, orta napı Orta-Geç Devoniyen yaşlı Keban mermerleri ile Geç Devoniyen yaşlı Delimehmet formasyonu ve en üstteki napı ise Erken Karbonifer yaşlı Süleymanlı formasyonu oluşturmaktadır. Ayrıca orta ve üst nap içinde yeşil renkli metadiyabazlardan oluşan Triyas öncesi yaşlı metabazik arakatkılar da gözlenmiştir. Bölgesel deneştirmeler Keban metamorfitlerinin Bolkardağı Birliği’nin eşdeğeri olabileceğini göstermektedir. Keban metamorphic rocks, located in Eastern Taurides, consist of platforms type carbonate and clastic rocks, regionally metamorphosed in greenschist facies. The age of the Keban metamorphites was based on two fossil findings (Glomospira and Ammodiscus family) which of the microorganism species were not detected and they were observed in only one location in Zeryandere, Permian aged estimated. The other formations of the metamorphic sequence were correlated with it. The age for the Keban metamorphites has been proposed as Permo-Triassic/Permo-Carboniferous up to now. All geological evaluations of the region were based on these ages. For the first time in this study, trace fossils (vermes trace) like Planolites, Rhizocorallium and Thalassinoides have been observed extensively. These fossils were detected on the layer surfaces of the Gogodere stratified dolomitic-crystallized limestone which is a member of Nimri formation, represents the medium level of the Keban metamorphites. The limestone levels include these trace fossils correspond to a typical “vermicular limestone facies”, representing Early-Middle Triassic (Scythian-Anisian) in Taurides. Allochthonous Keban metamorphic rocks consist of several nappes which overlaid by the others. There are three nappes in the study area; the lower nappe is constitute Early Triassic-Jurassic Nimri formation, the middle nappe is constitute Late Devonian Keban marbles and Delimehmet formation and the upper nappe is Early Carboniferous Süleymanlı formation. Also metabasic intercalations consisting green metadiabases pre-Triassic aged are observed in the middle and upper nappes. The regional correlations propose that the Keban metamorphites are equivalent of the Bolkardağı Union.

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    Pamukkale University Journal of Engineering Sciences
    Article . 2016 . Peer-reviewed
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      Pamukkale University Journal of Engineering Sciences
      Article . 2016 . Peer-reviewed
      Data sources: Crossref
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      DOAJ
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  • image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    Authors: Kazanci, N.; Karadenizli, L.; Seyitoǧlu, G.; Sen, S.; +4 Authors

    The Akkaşdaǧι area, situated in the southern margin of the Tertiary Çankιrι-Çorum Basin, Central Anatolia, Turkey, includes a 280 m thick, mostly continental sediment sequence that overlies either marine Palaeogene transgressive deposits or metamorphic rocks of Kirşehir Massif. From bottom to top the sequence can be divided into units of Deliceirmak Fm. (alluvial fan deposits) and Ceritkale member (marine fan-delta and shelf carbonates) of mid-upper Eocene, Güvendik Fm. (gypsum) of Oligocene, and Akkaşdaǧι Fm. (fine to coarse-grained alluvial clastics and lacustrine limestone) of upper Miocene-lower Pliocene. A granitic intrusion was emplaced into the basin after late Eocene. The Neogene succession includes mammalian fossils and the lithological composition of the succession is rather different from its equivalences in other parts of the basin. By facies analysis die Neogene infill could be categorised into alluvial fan deposits (facies association I), fluvial deposits (facies association II), lacustrine deposits (facies association III) and pyroclastic flow deposits (facies association IV). Facies association I is dominant and the others are observed inside as alternating sequences. The facies architecture and facies associations suggest that a structural depression existed in the area and was filled with sediments of distal alluvial fans, flood plains and lakes receiving deposits of distal or terminal alluvial fans and flood plains, and occupied partly by lakes. © Publications Scientifiques du Muséum national d'Histoire naturelle, Paris.

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    Authors: Özpınar, Yahya; Hançer, Mete; Semiz, Barış;

    In this region, marine, continental and lacustrine clay deposits which are used as a raw material in the cement sector were investigated. It is seen that Upper Cretaceous-Upper Eocene shales representing marine deposition are found in Malidagi in economic quantities, However, their Na(2)O% and K(2)O% contents are higher than in other clays. The Oligocene aged Bayiralan clay representing marine deposition have abundant magnesian minerals. Because of its high MgO% content, this clay is not suitable cement standard. The areal extent of the Upper Miocene-Lower Pliocene Kizilburun clays represented fine sediments in the floodplain are widely situated. These may be used in cement sector, but the have reserve and environmental problems. The red coloured clays belonging to the Pliocene Sakizcilar Formation are sutitable for cement standard. To decreasing the transportation costs of the Denizli cement factory, the Malidagi clay and Sakizcilar clay may be used together in different proportions, If the Malidagi and Sakizcilar clays may be used, the contents of K(2)O% and Na(2)O% will decrease.

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  • image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
    Authors: Wesselingh, F.P.; Alçiçek, Hülya;

    Abstract: We present the first record of the cardiid genus Monodacna from the Pliocene of Anatolia, Turkey. Monodacna imrei sp. nov. was found in the Pliocene Killik Formation from the western margin of the Baklan Basin, in very marginal brackish to freshwater lacustrine deposits. The new record extends the stratigraphic range of the modern Ponto-Caspian genus back into the Pliocene and adds to earlier evidence that modern Ponto-Caspian taxa originated in the Pliocene of south-western Turkey. © The Palaeontological Association.

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    Authors: Billi, A.; Berardi, G.; Gratier, J.-P.; Rossetti, F.; +7 Authors

    In our previous paper (Billi et al., 2017), using field geological observations, U-Th dating, and stable isotope analyses, we studied two deposits of Pleistocene thermogene travertines from Tuscany in central Italy. We concluded our study (1) warning that the common stratigraphic concept of travertine being a sedimentary succession with age younging from bottom to top is not always correct, (2) demonstrating that CaCO3 mineralization and veins can develop within the travertines after their formation with this syn-diagenetic process being able to modify the continuous bottom-up age evolution, and (3) showing that this post-depositional mineralization-veining process can not only modify the temporal succession but also deform and change the initial depositional travertine structure and its petrophysical properties. These conclusions could potentially make the interpretation of a travertine series more difficult than commonly thought. Alcicek et alii questioned our conclusions claiming that the travertine structures that we observed in Tuscany and interpreted as post-depositional features should have been interpreted, in analogy to similar structures from travertines elsewhere, as primary structures. Although we recognize, as already thoroughly stated in Billi et al. (2017), that the travertine depositional/post-depositional processes generally require further studies, we reaffirm the validity of our original interpretation at least for the structures analyzed in our previous paper. We, therefore, counter all criticisms by Alcicek et alii and conclude by indicating the way forward to further explore the depositional and post-depositional processes of thermogene travertines. © 2017 Elsevier B.V.

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    Authors: Alcicek, Mehmet Cihat; Mayda, Serdar; Titov, Vadim V.;

    The Burdur Basin is one of the NE-trending extensional orogen-top basins of SW Anatolia hosting alluvial-fan, fluvial and lacustrine deposits from the Late Miocene onward. The remains of Equus (Allohippus) sp., Paracamelus cf. gigas, and medium-sized deer (Cervidae gen. indet.) from the uppermost reach of the basin-fill succession show an interregional palaeobiogeographical linkage. The composition of fossil associations is typical for the wVillafranchian of eastern Europe and central Asia. The architecture of the basin-fill stratigraphy and associated fossil taxa refines the Early Pleistocene regional palaeogeography and biodiversity of Anatolia drawn over the Eurasian migration pattern. (C) 2012 Academie des sciences. Published by Elsevier Masson SAS. All rights reserved. The study was supported by international bilateral cooperation between The Scientific and Technological Research Council of Turkey and the Russian Foundation for Basic Research (TUBITAK-RFBR 111Y192 grant). MCA thanks the Turkish Academy of Sciences given the Outstanding Young Scientist Award, SM thanks the Ege University projects TTM/001/2010, TTM/002/2011 and VVT thanks the RFBR projects 12-05-91372-ST-a, 12-04-01691-a. Comments by Andrea Brogi and one anonymous reviewer are much appreciated. We wish to thank T.Tanju Kaya (Ege Univ.) and Hulya Alcicek (Pamukkale Univ.) for field help. Scientific and Technological Research Council of TurkeyTurkiye Bilimsel ve Teknolojik Arastirma Kurumu (TUBITAK); Russian Foundation for Basic ResearchRussian Foundation for Basic Research (RFBR) [TUBITAK-RFBR 111Y192]; Turkish Academy of SciencesTurkish Academy of Sciences; Ege UniversityEge University [TTM/001/2010, TTM/002/2011]; RFBRRussian Foundation for Basic Research (RFBR) [12-05-91372-ST-a, 12-04-01691-a] WOS: 000315702600001

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    Authors: Mehmet Cihat Alçiçek; Nizamettin Kazanci; Mehmet Özkul;

    The neotectonic development of western Anatolia was characterized by the formation of numerous graben-type basins, which have been well documented by general mapping, although the cause and timing of the Neogene regional tectonic extension remain controversial. Previous interpretations of the origin and evolution of these Neogene basins were based mainly on regional-scale tectonic inferences, rather than detailed basin-fill analysis. The present study of the terrestrial intramontane Çameli Basin in the western Taurides combines detailed facies analysis with biostratigraphic dating (mammalian and molluscan fossils) and documents three pulses of crustal extension that are reflected in changes in the palaeogeography and sedimentary architecture of the basin. Development of the Çameli graben commenced in the Vallesian time (early Tortonian), and is marked by alluvial-fan, fluvial and lacustrine depositional systems, with freshwater molluscan fauna. A second pulse of tectonic extension occurred in the late Ruscinian time (early-middle Pliocene), producing a new normal fault that split the basin longitudinally into two compartments. The lake environment expanded and deepened, coastal peat-forming mires developed and abundant mammal fauna appeared by the early Villanian time (middle Pliocene), with the lacustrine deposits onlapping the basin-margin and intrabasinal fault escarpments. The lacustrine environment subsequently shrank, as the progradation of axial river deltas and basin-margin fan deltas caused water shallowing and shoreline regression. A third pulse of extension occurred at the end of Villanian time (late Pliocene), when the development of a new generation of normal faults further split the basin into still narrower half-graben compartments. The third pulse of rifting is estimated to have accounted for little more than 10% of the sub-basinal crustal extension, but caused the most striking changes in the basin palaeogeography and drainage pattern. The inward development of the successive normal faults indicated a high-rate crustal extension. This is the first regional case study of a terrestrial neotectonic graben employing detailed sedimentary facies analysis and mammal biostratigraphy and providing a time-stratigraphic framework for the rifting pulses in western Anatolia. © 2004 Elsevier B.V. All rights reserved.

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    Sedimentary Geology
    Article . 2005 . Peer-reviewed
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      Sedimentary Geology
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    Authors: Alçiçek, Mehmet Cihat.;

    The Eşen Basin of southwestern Anatolia formed as a NE-trending intramontane extensional graben, ca. 15 km wide and 30 km long, in the Early Tortonian, after the southeasterly emplacement of the Lycian nappes during the Tauride orogeny. The basin originated due to gravitational collapse of the hinterland zone of the Lycian Taurides in response to the lithospheric thickening caused by microcontinent collision. Sedimentation commenced with the development of basin-margin alluvial fans and a southward-directed axial fluvial system, the latter expanding laterally, changing its channel pattern from braided to meandering and forming floodplain lakes. The isolated ephemeral lakes merged into a single lake at the basin centre, fringed with vegetated mires and desiccated by the end of Miocene time. The second pulse of rifting in the basin, dated to the Early Pliocene, is attributed to the roll-back and outward expansion of the Cretan subduction arc to the south. A new lake rapidly expanded, and the Pliocene deposition of a thick marly succession was terminated by the basinward advance of Gilbert-type deltas and gradual desiccation of the lake in the Late Pliocene. The third pulse of rifting, near the end of the Pliocene, formed new faults, tilted the basin-fill succession and records regional deformation due to the westward tectonic expulsion of the Anatolian craton. The base of the overlying Pleistocene alluvium is an angular unconformity, with fluvial terraces indicating considerable Quaternary uplift. The developmental stages of the Eşen Basin are consistent with the tectonostatigraphic evolution of the adjacent Çameli Basin to the north, which may thus serve as a reference framework for the tectonic history of the region's extensional grabens. © 2007 Elsevier B.V. All rights reserved.

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    Sedimentary Geology
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    Authors: Wesselingh, F.P.; Alçiçek, Hülya; Magyar, I.;

    We report on a Late Miocene mollusc fauna from a single locality in the Denizli Basin in Southwestern Turkey that is composed of ten presumably euryhaline species and three freshwater species. The fauna is remarkably distinct from faunas of the adjacent Late Miocene Aegean and Euxinian Basins, and has elements in common with the modern Caspian Sea fauna in the form of Didacna species. The Suggested age of the fauna (Late Miocene) would extend the stratigraphic range of the lymnocardiid genus Didacna (hitherto Calabrian-Extant) considerably. The palaeobiogeographic significance of the Denizli fauna is discussed. (C) 2008 Elsevier Masson SAS. All rights reserved.

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    Geobios; Pamukkale GCRIS Database
    Article . 2008 . Peer-reviewed
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    Authors: Ezher Toker; Mine Sezgül Kayseri-Özer; Mehmet Özkul; Sándor Kele;

    AbstractTravertine deposits in western Turkey are very well‐exposed in the area of Kocabaş, in the eastern part of the Denizli Basin. The palaeoclimatic significance of these travertines is discussed using U/Th dates, stable isotope data and palynological evidence. The Kocabaş travertine occurrences are characterized by successions of depositional terraces associated with palaeosols and karstic features. The travertines have been classified into eight lithotypes and one erosional horizon, namely: laminated, coated bubble, reed, paper‐thin raft, intraclasts, micritic travertine with gastropods, extra‐formational pebbles and a palaeosol layer. The analysed travertines mostly formed between 181 ka and 80 ka (Middle to Late Pleistocene) during a series of climatic changes including glacial and interglacial intervals; their δ13C and δ18O values indicate that the depositional waters were mainly of basinal thermal origin, occasionally mixed with surficial meteoric water. Palynological results obtained from the palaeosols showed an abundance of non‐arboreal percentage and xerophytic plants (Oleaceae and Quercus evergreen type) indicating that a drought occurred. Marine Isotope Stage 6 is represented by grassland species but Marine Isotope Stage 5 is represented by Pinaceae–Pinus and Abies, Quercus and Oleaceae. Uranium/thorium analyses of the Kocabaş travertines show that deposition began in Marine Isotope Stage 6 (glacial) and continued to Marine Isotope Stage 4 (glacial), but mostly occurred in Marine Isotope Stage 5 (interglacial). The travertine deposition continued to ca 80 ka in the south‐west of the study area, in one particular depression depositional system. Palaeoenvironmental indicators suggest that the travertine depositional evolution was probably controlled by fault‐related movements that influenced groundwater flow. Good correlation of the stable isotope values and dates of deposition of the travertines and palynological data of palaeosols in the Kocabaş travertines serve as a starting point for further palaeoclimate studies in south‐west Turkey. Additionally, the study can be compared with other regional palaeoclimate archives.

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    Sedimentology
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    Authors: Kaya, Ali;

    Doğu Toroslar’da yer alan Keban Metamorfitleri, yeşilşist fasiyesinde bölgesel metamorfizmaya uğramış platform tipi karbonat ve kırıntılı kayaçlardan oluşur. Keban metamorfitlerinin yaşı, Zeryanderedeki tek bir lokasyonda gözlenen ve Permiyen yaşlı olduğu tahmin edilen, türleri saptanamamış mikroorganizmalara ait iki fosil (Glomospira ve Ammodiscus familyasına ait fosiller) bulgusuna dayandırılmıştır. Metamorfik istifteki diğer formasyonlar da bu seviyeyle korele edilerek, Keban metamorfitleri için Permo-Triyas/Permo-Karbonifer yaşları önerilmiş ve şimdiye kadar kullanılmıştır. Bölgenin bütün jeolojik değerlendirmeleri de bu yaşlara göre yapılmıştır. İlk defa bu çalışmada, çok yaygın bir şekilde Planolites, Rhizocorallium ve Thalassinoides gibi iz fosiller gözlenmiştir. Bu iz fosiller, Keban metamorfitlerinin orta seviyelerini temsil eden Nimri formasyonuna ait Gogodere tabakalı dolomitik-kristalize kireçtaşı üyesinin tabaka üst yüzeylerinde tespit edilmiştir. Bu iz fosilleri içeren kireçtaşı seviyeleri, Toroslar’da Erken-Orta Triyas’ı (Skitiyen-Anisiyen) temsil eden tipik “vermiküler kireçtaşı fasiyesi”ne karşılık gelmektedir. Allokton konumlu Keban metamorfitleri, birbirlerini üzerleyen birkaç naptan oluşmaktadır. Çalışma alanı içinde üç nap vardır; en alt napı Erken Triyas-Jura yaşlı Nimri formasyonu oluşturur, orta napı Orta-Geç Devoniyen yaşlı Keban mermerleri ile Geç Devoniyen yaşlı Delimehmet formasyonu ve en üstteki napı ise Erken Karbonifer yaşlı Süleymanlı formasyonu oluşturmaktadır. Ayrıca orta ve üst nap içinde yeşil renkli metadiyabazlardan oluşan Triyas öncesi yaşlı metabazik arakatkılar da gözlenmiştir. Bölgesel deneştirmeler Keban metamorfitlerinin Bolkardağı Birliği’nin eşdeğeri olabileceğini göstermektedir. Keban metamorphic rocks, located in Eastern Taurides, consist of platforms type carbonate and clastic rocks, regionally metamorphosed in greenschist facies. The age of the Keban metamorphites was based on two fossil findings (Glomospira and Ammodiscus family) which of the microorganism species were not detected and they were observed in only one location in Zeryandere, Permian aged estimated. The other formations of the metamorphic sequence were correlated with it. The age for the Keban metamorphites has been proposed as Permo-Triassic/Permo-Carboniferous up to now. All geological evaluations of the region were based on these ages. For the first time in this study, trace fossils (vermes trace) like Planolites, Rhizocorallium and Thalassinoides have been observed extensively. These fossils were detected on the layer surfaces of the Gogodere stratified dolomitic-crystallized limestone which is a member of Nimri formation, represents the medium level of the Keban metamorphites. The limestone levels include these trace fossils correspond to a typical “vermicular limestone facies”, representing Early-Middle Triassic (Scythian-Anisian) in Taurides. Allochthonous Keban metamorphic rocks consist of several nappes which overlaid by the others. There are three nappes in the study area; the lower nappe is constitute Early Triassic-Jurassic Nimri formation, the middle nappe is constitute Late Devonian Keban marbles and Delimehmet formation and the upper nappe is Early Carboniferous Süleymanlı formation. Also metabasic intercalations consisting green metadiabases pre-Triassic aged are observed in the middle and upper nappes. The regional correlations propose that the Keban metamorphites are equivalent of the Bolkardağı Union.

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