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The Tauride Ophiolites of Anatolia(Turkey):A Review

Journal of Earth Science 2016年第6期27卷 901-934页

作者： osman parlak Cukurova On Universitesi Jeoloji Muhendisligi Bolumu Balcah Adana 01380 Turkey

The Tauride ophiolites lie on the northern and southern flanks of an E-W-trending Tanride carbonate platform. They mainly consist of three tectonic units namely in ascending order, ophiolitic melange, sub-ophiolitic metamorphic sole and oceanic lithospheric remnants. They were generated above intra-oceanic subduction zones and emplaced over the Tauride carbonate platform from different Neotethyan oceanic basins in the Late Cretaceous. Tauride ophiolites from west to east are described and reviewed. All are underlain by well-preserved dynamothermal metamorphic soles of varied structural thicknesses up to 500 m that have a constant structural position between ophiolitic melange below and harzburgitic mantle tectonites above and display typical inverted metamorphic sequences from amphibolite facies above to greenschist facies below. The metamorphic soles are shown to have evolved during the initiation of subduction and emplacement processes. In the PozantlKarsantl area the contact between the metamorphic sole and the overlying serpentinized harzburgites is characterized by a 1.5-2-m-thick zone of sheared serpentinized harzburgitic mantle intercalated with amphibolites and cut by thick mafic dykes （7-8 m） which postdate intraoceanic metamorphism and high-temperature ductile deformation. This contact is interpreted as an intra-oceanic decoupling surface along which volcanics from the upper levels of the down-going plate were metamorphosed to amphibolite facies and accreted to the base of the hanging wall plate. The metamorphic soles and overlying ophiolitic rocks were intruded by numerous isolated post-metamorphic diabase dykes filled by island arc tholeiitic magma. Subduction initiation and roll-back processes best explain the structural and petrological relationships of Late Cretaceous ophiolite genesis, metamorphic sole formation and subsequent dyke emplacement of the Tauride ophiolites.

关键词： ophiolite metamorphic sole dyke emplacement roll-back subduction initiation.

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Age and duration of intra-oceanic arc volcanism built on a suprasubduction zone type oceanic crust in southern Neotethys,SE Anatolia

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Geoscience Frontiers 2013年第4期4卷 399-408页

作者： Fatih Karaoglan osman parlak Urs Kltzli Friedrich Koller Tamer Rizaoglu Cukurova niversitesi.Jeoloji Mhendisligi Blm 01330 Balcali.Adana.Turkey University of Vienna.Centre for Earth Sciences Kahramanmaras Stc Imam niversitesi Jeoloji Mhendisligi Blm46100 KahramanmarasTurkey

The southeastern Anatolia comprises numbers of tectono-magmatic]stratJgraphic units such as the metamorphic massifs, the ophiolites, the volcanic arc units and the granitoid rocks. All of them play important role for the late Cretaceous evolution of the southern Neotethys. The spatial and temporal relations of these units suggest the progressive development of coeval magmatism and thrusting during the late Cretaceous northward subduction/accretion. Our new U-Pb zircon data from the rhyolitic rocks of the wide-spread volcanic arc unit show ages of （83.1 ± 2.2）-（74.6 ± 4.4） Ma. Comparison of the ophiolites, the volcanic arc units and the granitoids suggest following late Cretaceous geological evolution. The ophiolites formed in a suprasubduction zone （SSZ） setting as a result of northward intra-oceanic subduction. A wide-spread island-arc tholeiitic volcanic unit developed on the top of the SSZ-type crust during 83 75 Ma. Related to regional plate convergence, northward under-thrusting of SSZ-type ophiolites and volcanic arc units was initiated beneath the Tauride platform （Malatya-Keban） and followed by the intrusion of I-type calc-alkaline volcanic arc granitoids during 84 82 Ma. New U-Pb ages from the arc-related volcanic-sedimentary unit and granitoids indicate that under-thrusting of ophiolites together with the arc-related units beneath the Malatya-Keban platform took place soon after the initiation of the volcanic arc on the top of the SSZ- type crust. Then the arc-related volcanic-sedimentary unit continued its development and lasted at - 75 Ma until the deposition of the late Campanian-Maastrichtian shallow marine limestone. The subduction trench eventually collided with the Bitlis-Pfitfirge massif giving rise to HP-LT meta- morphism of the Bitlis massif. Although the development of the volcanic arc units and the granitoids were coeval at the initial stage of the subduction/accretion both tectono-magmatic units were genetically different from each other.

关键词： Island-arcOphioliteGranitoidU-Pb geochronologySSZ settingSE Anatolia

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Petrology of ultramafic to mafic cumulate rocks from the G?ksun(Kahramanmaras) ophiolite,southeast Turkey

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Geoscience Frontiers 2020年第1期11卷 109-128页

作者： osman parlak Utku Bagcı Tamer Rızaoglu Corina Ionescu GüzideÖnal Volker Höck Hüseyin Kozlu Çukurova Universitesi Jeoloji Mühendisligi BölümüBalcalıTR-01330 AdanaTurkey State Key Laboratory of Geological Processes and Mineral Resources Center for Global TectonicsSchool of Earth SciencesChina University of GeosciencesWuhan 430074China Mersin Universitesi Jeoloji Mühendisligi BölümüÇiftlikköyTR-33343 MersinTurkey Kahramanmaras¸SütçüImam Universitesi Jeoloji Mühendisligi BölümüAvs¸ar KampüsüTR-46100 KahramanmarasTurkey Babes-Bolyai University Geology Department1 Kogalniceanu Str.RO-400084 Cluj-NapocaRomania Kazan(Volga Region)Federal University Archeotechnologies&Archeological Material Sciences Laboratory18 Kremlevskaya Str.420000 KazanRussia University of Salzburg Division of Geography and Geology34 Hellbrunner Str.A-5020 SalzburgAustria Türkiye Petrolleri Anonim Ortaklıgı TR-06520 AnkaraTurkey

The G?ksun(Kahramanmaras)ophiolite(GKO),cropping out in a tectonic window bounded by the Malatya metamorphic unit on both the north and south,is located in the EW-trending lower nappe zone of the southeast Anatolian orogenic belt(Turkey).It exhibits a complete oceanic lithospheric section and overlies the Middle Eocene Maden Group/Complex with a tectonic contact at its *** ophiolitic rocks and the tectonically overlying Malatya metamorphic(continental)unit were intruded by I-type calc-alkaline Late Cretaceous granitoid(~81-84 Ma).The ultramafic to cumulates in the GKO are represented by wehrlite,plagioclase wehrlite,olivine gabbro and *** crystallization order for the cumulate rocks is as follows:olivine±chromian spinel→clinopyroxene→*** major and trace element geochemistry as well as the mineral chemistry of the ultramafic to mafic cumulate rocks suggest that the primary magma generating the GKO is compositionally similar to that observed in the modern island-arc tholeiitic *** mineral chemistry of the ultramafic to mafic cumulates indicates that they were derived from a mantle source that was previously depleted by earlier partial melting *** highly magnesian olivine(Fo77-83),clinopyroxene(Mg#of 82-90)and the highly Ca-plagioclase(An81-89)exhibit a close similarity to those,which formed in a supra-subduction zone(SSZ)*** field and the geochemical evidence suggest that the GKO formed as part of a much larger sheet of oceanic lithosphere,which accreted to the base of the Tauride active continental margin,including the ispendere,K?mürhan and the Guleman *** latter were contemporaneous and genetically/tectonically related within the same SSZ setting during the closure of the Neotethyan oceanic basin(Berit Ocean)between the Taurides to the north and the Bitlis-Pütürge massif to the south during the Late Cretaceous.

关键词： Göksun(Kahramanmaras)ophiolite Cumulate SSZ-Spreading Neotethys Late Cretaceous SE Anatolia

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Epidemic management in a measles outbreak in 2023,the return of vaccine-preventable diseases:A single center,retrospective observational study

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Asian Pacific Journal of Tropical Medicine 2024年第3期17卷 110-118页

作者： Sevgi Aslan Tuncay Gulsen Akkoc Seyhan Yilmaz Burcu parlak Pinar Canizci Erdemli Aylin Dizi Isik Didem Buyuktas Aytac Meryem Cagla Abaci Capar Eda Kepenekli Kadayifci Marmara University Faculty of Medicine Department of Pediatric Infectious DiseaseIstanbulTurkey

Objective:To investigate the importance of immunization in preventing measles infection and to determine the most useful laboratory tests for confirmation of ***:This study included pediatric cases evaluated with a presumed diagnosis of measles between December 2022 and June 2023,at Marmara University Pendik Training and Research *** effects of vaccination status and underlying disease on the clinical course,treatments,and complications were ***:In total,117 patients were enrolled in the study with a median age of 80 months(IQR:32.5-125.0).Twelve patients with contact history were asymptomatic and had an underlying disorder,and intravenous immunoglobulin was given to them for post-exposure ***-one patients had confirmed measles *** treatment was given to three patients(a newborn,a girl with rhabdomyosarcoma,and a healthy boy)with respiratory ***-eight percent of confirmed measles cases were unvaccinated,and all hospitalized cases were unvaccinated or *** full-vaccinated children had confirmed measles *** PCR from nasopharyngeal swabs was negative in all of them,and their diagnosis was established with anti-measles IgM ***:The measles vaccine is the most effective way to protect from measles and measles-related *** measles can also occur in fully vaccinated patients,the disease is milder than in unvaccinated *** ELISA and RT-PCR tests together may be beneficial in patients with high clinical suspicion for early diagnosis.

关键词： Measles Outbreak Vaccination Vitamin A Ribavirin

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土耳其中部／东部，从黑海（欧亚大陆）到阿拉伯边缘（Gondwana）：相互作用和合成

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海洋地质 2008年第3期24卷 79-80页

作者： Alastair Robertson Yuksel Metin osman parlak Samuel Rice Tamer Rizaoglu Timur Ustaome 万荣胜（译）万玲（校对）英国地球科学学院土耳其MTA 土耳其阿德亚曼大学英国CASP 土耳其阿克萨赖大学不详

作为对整个造山带合成的一个贡献，我们已经确定和解释了暴露于在土耳其中部／东部，从黑海到阿拉伯地台的地层单元。从：ILN南，从上往下，主要的构造单元是：Pontides（欧亚边缘）；北边的海洋线性构造；Gurun，Munzur和Keban—Malaty... 详细信息

作为对整个造山带合成的一个贡献，我们已经确定和解释了暴露于在土耳其中部／东部，从黑海到阿拉伯地台的地层单元。从：ILN南，从上往下，主要的构造单元是：Pontides（欧亚边缘）；北边的海洋线性构造；Gurun，Munzur和Keban—Malatya地台；中部的蛇绿岩线性构造；Bitlis—Ptrge断块；南部的蛇绿岩线性构造；阿拉伯大陆边缘。

关键词：阿拉伯土耳其相互作用欧亚大陆合成黑海线性构造地层单元

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Clonal propagation of mastic tree(Pistacia lentiscus *** Duham.) in outdoor beds using different rootstock and grafting techniques

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Journal of Forestry Research 2018年第4期29卷 1052-1058页

作者： Salih parlak Department of Forest Engineering Faculty of ForestryBursa Technical University

We assessed different rootstocks and grafting techniques to clonally propagate mastic tree （Pistacia lentiscus var. chia）. Mastic tree is a dioecious tree but the quantity and quality of the resin secreted by female trees are very low; therefore, male trees that are clonally propagated are used to establish commercial plantations for mastic production. Conventional long branch cuttings for clonal production requires too much materials and has a very low rooting rate. Rooting with tissue culture and green cuttings has also failed outdoors. Grafting of mastic on other Pistacia species has not been tried so far; therefore, this study was aimed at developing grafting methods for the clonal propagation of mastic. P. atlantica and P. lentiscus rootstocks were grafted from 15 February to 15 October every 15 days using three grafting methods and a two-factor randomized block trial design. Early spring （15 February-15 March） proved to be the best time for grafting using either of the rootstocks. The highest grafting success was attained using the scions grafted on P. atlantica from 15 February to 15 March. The best bud-burst percentage was obtained using P. atlantica and P. lentiscus rootstocks.

关键词： Pistacia lentiscus var chia Grafting Budding Rootstock

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Zeolite usage as source of silica to produce cordierite in MgO–Al_2O_3–SiO_2 system

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Journal of Advanced Ceramics 2018年第4期7卷 370-379页

作者： Tu?ba Tun? parlak A.?ükran DEMIRKIRAN Department of Metallurgical and Materials Engineering Faculty of EngineeringSakarya UniversityEsentepe Campus

In this study, natural zeolite was used as source of silica to produce cordierite. MgO and Al_2O_3 were added to zeolite to obtain the cordierite stoichiometry. Mixture of these raw materials was mechanically activated for different durations. The mechanically activated powder mixture was characterized using XRD, DSC, SEM, specific surface area, and particle size analyzer. The pycnometer method was used to measure the densities of mechanically activated powder mixtures. Mechanically activated for 60 min powder mixture was sintered at 1150–1350 ℃ for 1 h. The sintering behavior of the samples was determined by measuring the linear shrinkage, density, and apparent porosity. The phases in the sintered samples were identified by XRD. Cordierite and spinel phases were detected for sintered at a temperature higher than 1150 ℃ but corundum accompanied to cordierite and spinel at 1150 ℃. The microstructure of the samples was examined using both SEM and AFM. The sintering behavior and microstructural properties of the samples changed with an increase in the sintering temperature. As the apparent porosity increased with increasing sintering temperature, linear shrinkage and density values decreased. Density values were determined as 2.31–2.69 g/cm^3 depending on the temperature. The grains coarsened at higher temperature and the average grain size depending on the temperature was 1.34–1.96 μm. From the results optimum sintering temperature was determined as 1250 ℃. Dense material was produced at a temperature as low as 1250 ℃ using zeolite as raw material.

关键词： mechanical activation sintering zeolite cordierite

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Vibrational investigation of 1-cyclopentylpiperazine:A combined experimental and theoretical study

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Science China(Physics,Mechanics & Astronomy) 2014年第9期57卷 1654-1661页

作者： BAGLAYAN zge KESAN Gürkan parlak Cemal ALVER zgür SENYEL Mustafa Department of Physics Science Faculty Anadolu University Institute of Physics and Biophysics Faculty of Science University of South Bohemia Department of Physics Dumlupinar University

FT-IR and Raman spectra of 1-cyclopentylpiperazine(1cppp)have been experimentally examined in the region of 4000–*** optimized geometric parameters,conformational equilibria,normal mode frequencies and corresponding vibrational assignments of 1cppp(C9H18N2)are theoretically examined by means of B3LYP hybrid density functional theory(DFT)method together with 6-31++G(d,p)basis *** the basis of potential energy distribution(PED)reliable vibrational assignments have been made and the thermodynamics functions,highest occupied and lowest unoccupied molecular orbitals(HOMO and LUMO)of 1cppp have been *** are employed for four different conformations in C1 and Cs point groups of 1cppp in gas *** between the experimental and theoretical results indicates that B3LYP method is able to provide satisfactory results for predicting vibrational frequencies and the structural parameters,vibrational frequencies and ***,C1(equatorial-axial)point group has been found as the most stable conformer of 1cppp.

关键词： 1-cyclopentylpiperazine vibrational spectra PED DFT B3LYP

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Investigation of post-thermal annealing on material properties of Cu-In-Zn-Se thin films

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Journal of Semiconductors 2017年第12期38卷 26-31页

作者： H.H.Güllü M.parlak Central Laboratory Middle East Technical University(METU)Ankara 06800Turkey Department of Physics Middle East Technical University(METU)Ankara 06800Turkey Center for Solar Energy Research and Applications(GUNAM) METUAnkara 06800Turkey

The Cu-In-Zn-Se thin film was synthesized by changing the contribution of In in chalcopyrite CulnSe2 with Zn. The XRD spectra of the films showed the characteristic diffraction peaks in a good agreement with the quaternary Cu-In-Zn-Se compound. They were in the polycrystalline nature without any post-thermal process, and the main orientation was found to be in the （112） direction with tetragonal crystalline structure. With increasing annealing temperature, the peak intensities in preferred orientation became more pronounced and grain sizes were in increasing behavior from 6.0 to 25.0 nm. The samples had almost the same atomic composition of ***2. However, EDS results of the deposited films indicated that there was Se re-evaporation and/or segregation with the annealing in the structure of the film. According to the optical analysis, the transmittance values of the films increased with the annealing temperature. The absorption coefficient of the films was calculated as around 105 cm-1 in the visible region. Moreover, optical band gap values were found to be changing in between 2.12 and 2.28 eV depending on annealing temperature. The temperature-dependent dark- and photo-conductivity measurements were carried out to investigate the electrical characteristics of the films.

关键词： annealing Cu-In-Zn-Se thin film

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Biliary endoscopic sphincterotomy: Techniques and complications

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World Journal of Clinical Cases 2018年第16期6卷 1073-1086页

作者： Ayd?n Seref Kksal Ahmet Tarik Eminler Erkan parlak Department of Gastroenterology Sakarya University School of Medicine Department of Gastroenterology Hacettepe University School of Medicine

Biliary endoscopic sphincterotomy(EST) refers to the cutting of the biliary sphincter and intraduodenal segment of the common bile duct following selective cannulation, using a high frequency current applied with a special knife, sphincterotome, inserted into the papilla. EST is either used solely for the treatment of diseases of the papilla of Vater, such as sphincter of Oddi dysfunction or to facilitate subsequent therapeutic biliary interventions, such as stone extraction, stenting, etc. It is a prerequisite for biliary interventions, thus every practitioner who performs endoscopic retrograde cholangiopancreatography needs to know different techniques and the clinical and anatomic parameters related to the efficacy and safety of the procedure. In this manuscript, we will review the indications, contraindications and techniques of biliary EST and the management of its complications.

关键词： Complication Indication Biliary endoscopic sphincterotomy Endoscopic retrograde cholangiopancreatography

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