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Articles 181 - 210 of 917
Full-Text Articles in Earth Sciences
Geochemical And Petrographic Approach For The Origin Of The Limestone Blocks Of Thewalls Of The Great Temple Of Hattusha, Çorum (N-Turkey), İsmai̇l Ömer Yilmaz, Andreas Schachner, İbrahi̇m Tonguç Uysal, Ezgi̇ Ünal İmer
Geochemical And Petrographic Approach For The Origin Of The Limestone Blocks Of Thewalls Of The Great Temple Of Hattusha, Çorum (N-Turkey), İsmai̇l Ömer Yilmaz, Andreas Schachner, İbrahi̇m Tonguç Uysal, Ezgi̇ Ünal İmer
Turkish Journal of Earth Sciences
The socle stones of the Great Temple in the Lower City of the Hittite capital city, Hattusha (Çorum Province) have been studied for the first time by petrographic and geochemical analysis (Sr isotope, stable isotope, and trace element geochemistry). Study objectives were to determine the carbonate facies of the stone samples used in the Great Temple and investigate their possible sources. Petrographic analysis of 10 limestone samples presents five clusters of different microfacies. Stable isotope (δ13C and δ18O) analysis displayed the presence of 5 groups in parallel with petrographic analysis. Trace element analysis of the same groups displayed considerable difference …
Stratigraphic Correlation Of The Givetian (Late Middle Devonian) Deposits In Qujing,Yunnan, Southwestern China And The Paleogeographic Implications, Jianhua Wang, Yunchuan Mi, Xiaorou Ma, Yukun Bi
Stratigraphic Correlation Of The Givetian (Late Middle Devonian) Deposits In Qujing,Yunnan, Southwestern China And The Paleogeographic Implications, Jianhua Wang, Yunchuan Mi, Xiaorou Ma, Yukun Bi
Turkish Journal of Earth Sciences
Detailed description of spatio-temporal framework of fossil-bearing strata is of fundamental significance for understanding the evolution of organisms and regional tectonics. The Qujing and Haikou formations are two lithological units exposed in eastern Yunnan, southwestern China, and both bear rich fossils indicative of a Middle Devonian age, while their relationship or lateral correlation remains unclear. Based on detailed observations of outcrops of these two formations in Qujing, eastern Yunnan, and as well as their typical rock characteristics and fossil contents, we propose that the two formations are basically contemporaneous heterotopic facies. From north to south of the Qujing area, the …
Skill Assessment Of A High Resolution (1/72 Degree) Black Sea Ocean Model, Bi̇lge Tutak
Skill Assessment Of A High Resolution (1/72 Degree) Black Sea Ocean Model, Bi̇lge Tutak
Turkish Journal of Earth Sciences
The skill of a high-resolution Black Sea circulation model (ROMS) is assessed using the available satellite and field data for Sea Surface Height Anomaly (SSHA), Sea Surface Temperature, and CTD profiles. The model is configured to simulate the 9-year period between 2012 and 2021. The model's skill is assessed using standard analytical methods for error calculation such as Root Mean Square Error (RMSE) and correlation. Additionally, the model results are assessed using several more recent methods such as the relative operating characteristic (ROC). The results show that the model is capable of simulating daily mean SSHA with an RMSE value …
The Active Fault Pattern Based On Morphotectonic And Structural Data In The South Ofulubat Lake And The Susurluk Valley Along The Southern Branch Of North Anatolian Faultzone: A Criticism Of The Bend Model In Northwest Anatolia, Gürol Seyi̇toğlu, Korhan Esat
The Active Fault Pattern Based On Morphotectonic And Structural Data In The South Ofulubat Lake And The Susurluk Valley Along The Southern Branch Of North Anatolian Faultzone: A Criticism Of The Bend Model In Northwest Anatolia, Gürol Seyi̇toğlu, Korhan Esat
Turkish Journal of Earth Sciences
Field observations and morphotectonic evaluations on the south of Ulubat Lake and the Susurluk valley show that the dominant active fault pattern consists of northeast-southwest and east northeast-west southwest right-lateral faults and northwestsoutheast normal faults developing between these strike-slip faults. We redefined the active faults in the south of Ulubat Lake and discovered that these northeast-southwest right-lateral faults control the route of Susurluk River. Based on these discoveries and evaluations, we can claim that the "bend model" previously proposed for the region is not valid, as seen in the Mustafakemalpaşa Fault and Balıkesir-Kepsut Fault examples. Instead, we suggest that the …
Further Contribution To The Early Miocene Woody Flora Of Galatian Volcanic Provincefrom Doğanyurt Village, Ankara (Turkey), Ünal Akkemi̇k, Stanila Iamandei, Hakan Çeli̇k
Further Contribution To The Early Miocene Woody Flora Of Galatian Volcanic Provincefrom Doğanyurt Village, Ankara (Turkey), Ünal Akkemi̇k, Stanila Iamandei, Hakan Çeli̇k
Turkish Journal of Earth Sciences
The Galatian Volcanic Province (GVP) located in central-north Anatolia had a rich woody flora. The purpose of the present study is to contribute to the early Miocene woody flora of the GVP from two fossil sites from Doğanyurt Village of the city of Beypazarı in the Province of Ankara. The fossil sites, which are near to each other, have small pieces of fossil woods. Total 16 fossil woods were collected from two neighbour sites. Three thin sections as transversal, tangential and radial sections from each sample were taken, and they were identified microscopically. As a result, ten fossil species were …
The Provenance Of Coarse-Grained Turbidite Sandstones In The Kırkgeçit Formation(Western Part Of The Elazığ Basin-East Turkey), Onur Alkaç, Ercan Aksoy
The Provenance Of Coarse-Grained Turbidite Sandstones In The Kırkgeçit Formation(Western Part Of The Elazığ Basin-East Turkey), Onur Alkaç, Ercan Aksoy
Turkish Journal of Earth Sciences
Modal analysis of sandstones for conglomerate rich marine basins is useful for investigating the provenance types surrounded by plate tectonics. Different kinds of siliciclastic rocks are important indicators for defining the paleogeography and geotectonic conditions of the sedimentary basin by provenance analysis. This paper, which focuses on the petrography and provenance of conglomerate rich turbidite systems, is one of the rarest studies on the sedimentary characteristics in the scientific literature. In this context, the study was carried out in the western part of the Elazığ Basin. The Middle Eocene?Oligocene basin infill called the Kırkgeçit Formation is characterised by the conglomerate …
Growth Of The Imbrication Zone Along The Southeast Anatolian Orogenic Belt: Evidencefrom Fission Track Thermochronology From Gölbaşı Region (Se Turkey), Yusuf Topak
Turkish Journal of Earth Sciences
One of the major components of continental collision zones is their imbricated zones. Such a zone along the Southeast Anatolian Orogenic Belt (SAOB) is solely controlled by a still-active convergence and accretion system between the Anatolian Plate and Arabian platform since at least Late Cretaceous. The zone is characterized by NEE/SWW-trending, northward-dipping thrust slices that are squeezed between the Tauride Block to the north and the Arabian platform to the south. The units cropping out within the zone comprise Neo-Tethysrelated magmatic, ophiolitic, sedimentary and metamorphic rocks with Late Cretaceous to Miocene formation/metamorphism ages. The Karanlıkdere granitoid intrudes into Late Cretaceous …
Updated Geochemical And Geothermometry Study On Ömer-Gecek Geothermal Area (Afyonkarahisar/Turkey), Can Başaran, Yusuf Ulutürk, Ahmet Yildiz
Updated Geochemical And Geothermometry Study On Ömer-Gecek Geothermal Area (Afyonkarahisar/Turkey), Can Başaran, Yusuf Ulutürk, Ahmet Yildiz
Turkish Journal of Earth Sciences
The Ömer-Gecek region, one of the most critical geothermal areas of Afyonkarahisar, together with Western Anatolia, serves as a model for the integrated use of geothermal waters. As a result of the analysis made on the samples collected from the newly drilled wells, the chemical composition of the Ömer-Gecek geothermal waters, with a max temperature of 125 °C, has been determined as Na-Cl. The primary hydrochemical process affecting the chemical composition is silicate weathering. All the applied geothermometer methods showed that the water's maximum reservoir temperature was 120-130 °C. The calcite, dolomite, and aragonite minerals tend to precipitate. When compared …
Holocene Sedimentary History Of South Danamandıra Lake: A Peatland In West Of İstanbul, Çatalca Peninsula, Nw Turkey, Özlem Makaroğlu, Melda Küçükdemi̇rci̇, Nurgül Karlioğlu, Dursun Acar, Ali̇ Gürel, Rüya Yilmaz Dağdevi̇ren, Nuretti̇n Yakupoğlu, Asen Sabuncu, Damla Şahi̇n Altun, Mustafa Ömer Karaöz, Memet Namik Çağatay
Holocene Sedimentary History Of South Danamandıra Lake: A Peatland In West Of İstanbul, Çatalca Peninsula, Nw Turkey, Özlem Makaroğlu, Melda Küçükdemi̇rci̇, Nurgül Karlioğlu, Dursun Acar, Ali̇ Gürel, Rüya Yilmaz Dağdevi̇ren, Nuretti̇n Yakupoğlu, Asen Sabuncu, Damla Şahi̇n Altun, Mustafa Ömer Karaöz, Memet Namik Çağatay
Turkish Journal of Earth Sciences
This study investigates the sedimentological evolution of the South Danamandıra Lake (SDL) lake in Çatalca Peninsula, 70 km west of İstanbul, using Georadar data and multiproxy analyses of five sediment cores. The lake is a 1.3-m deep, endorheic freshwater peatland, heavily colonised by common reed (Phragmites sp.). The multiproxy core investigations include a lithological core description and environmental magnetism, physical properties (gamma density and magnetic susceptibility), geochemical elemental, pollen and radiocarbon dating analyses. The lithological sequence in the lake consists of an upper peat unit and a lower sand-silt-clay unit. The peat unit is characterized by lower magnetic susceptibility, density …
Sedimentary Records Of Trace Elements Contamination In Sediment Core From The Gulf Of Gemlik, Marmara Sea, Turkey: History, Contamination Degree, And Sources, Tuğçe Nagi̇han Arslan Kaya, Erol Sari, Mehmet Ali̇ Kurt
Sedimentary Records Of Trace Elements Contamination In Sediment Core From The Gulf Of Gemlik, Marmara Sea, Turkey: History, Contamination Degree, And Sources, Tuğçe Nagi̇han Arslan Kaya, Erol Sari, Mehmet Ali̇ Kurt
Turkish Journal of Earth Sciences
The pollution history of aluminum (Al), chromium (Cr), cobalt (Co), lead (Pb), zinc (Zn), copper (Cu), and mercury (Hg) were evaluated using geochemical and sedimentological properties of two sediment cores. The MD22A contained a mass-flow unit and two coccolith units. The upper coccolith was characterized by high organic matter, but it was relatively depleted in terms of all studied elements, suggesting dilution by high inorganic carbon. In the mass-flow unit, the relatively high Cr, Co, Zn, and Hg levels suggested additional contamination sources from the Kocadere Stream and Kocasu River. The ranges of Al, Cr, Co, Cu, Hg, Pb, and …
A History Of Pistacia Lentiscus And Pinus Brutia Trees And Their Ecological Changes In The Güllük Bay (Muğla, Sw Turkey) During The Last 400 Years, Demet Bi̇lteki̇n, Georg Schwamborn, Kürşad Kadi̇r Eri̇ş, Dursun Acar, Bi̇kem Ekberzade, Zahra Hashemi̇, Nuretti̇n Yakupoğlu, Ali̇ Mohammadi̇, Ömer Yetemen
A History Of Pistacia Lentiscus And Pinus Brutia Trees And Their Ecological Changes In The Güllük Bay (Muğla, Sw Turkey) During The Last 400 Years, Demet Bi̇lteki̇n, Georg Schwamborn, Kürşad Kadi̇r Eri̇ş, Dursun Acar, Bi̇kem Ekberzade, Zahra Hashemi̇, Nuretti̇n Yakupoğlu, Ali̇ Mohammadi̇, Ömer Yetemen
Turkish Journal of Earth Sciences
In this study, we present pollen records together with a multiproxy analysis from a sediment core collected from the Güllük Bay (Bargilya Cove, Muğla, SW Turkey), covering the last 400 years. Pistachio shrubland was occupying around the Güllük Bay between 1613 and 1741 AD. However, after 1741 AD, the vegetation canopy suddenly changed and Turkish pine (Pinus brutia) was established. This supports that the main factor affecting the expansion of Pistacia lentiscus was precipitation rather than temperature after 1741 AD. This change is also indicated by high Sr-Ca values, reflecting arid conditions. Two anthropogenic phases developed in the region. The …
Tectonomagmatic Reconstruction Of The Upper Mesozoic-Cenozoic Neotethyan Arcs In The Lut Block, East Iran: A Review And Synthesis, Reza Arjmandzadeh, Saeed Alirezaei, Alireza Almasi
Tectonomagmatic Reconstruction Of The Upper Mesozoic-Cenozoic Neotethyan Arcs In The Lut Block, East Iran: A Review And Synthesis, Reza Arjmandzadeh, Saeed Alirezaei, Alireza Almasi
Turkish Journal of Earth Sciences
The Lut Block in east Iran with a widespread record of arc-type Mesozoic-Cenozoic magmatic rocks is bordered by the Birjand (Sistan) ophiolitic assemblage to the east and the Sabzevar ophiolitic assemblage to the north. The nature and tectonomagmatic setting of these sutures and associated arcs are controversial. The geochemical attributes of the Upper Cretaceous-Paleogene intrusive and extrusive rocks in the central (CLB) and the northern Lut block (NLB) and in the Sabzevar ophiolite zone (SOZ), Late Cretaceous calc-alkaline and adakitic rocks to the east of the Sistan suture (CAS), and the Bazman intrusives to the west are consistent with a …
Devonian Parathuramminids From Taurides, Southern Turkey, Recep Özkan
Devonian Parathuramminids From Taurides, Southern Turkey, Recep Özkan
Turkish Journal of Earth Sciences
Devonian shallow marine carbonate rocks of the Taurides (southern Turkey) host rich and diverse faunal assemblages of foraminifera including unilocular organisms of the family Parathuramminidae. This study allowed investigating the calcareous unilocular parathuramminid fauna obtained from three measured stratigraphic sections Halevikdere, Kocadere and Eceli in addition to one detailed, shorter section measured along the Halevikdere section. The investigation revealed that the parathuramminid species, which commonly occur in lagoonal environments, are widely distributed throughout the studied sections. They mostly exist in limestone beds deposited in a time interval from Middle Devonian (Eifelian) to Late Devonian (Frasnian). However, their richness and diversity …
Determination Of Recent Tectonic Deformations Along The Tuz Gölü Fault Zone In Centralanatolia (Turkey) With Gnss Observations, Cemi̇l Gezgi̇n, Semi̇h Ekerci̇n, İbrahi̇m Ti̇ryaki̇oğlu, Bahadir Aktuğ, Hedi̇ye Erdoğan, Esra Gürbüz, Osman Orhan, Süleyman Sefa Bi̇lgi̇li̇oğlu, Ahmet Tarik Torun, Hali̇l İbrahi̇m Gündüz, Osman Oktar, Cezmi̇ Türkmen, Efdal Kaya
Determination Of Recent Tectonic Deformations Along The Tuz Gölü Fault Zone In Centralanatolia (Turkey) With Gnss Observations, Cemi̇l Gezgi̇n, Semi̇h Ekerci̇n, İbrahi̇m Ti̇ryaki̇oğlu, Bahadir Aktuğ, Hedi̇ye Erdoğan, Esra Gürbüz, Osman Orhan, Süleyman Sefa Bi̇lgi̇li̇oğlu, Ahmet Tarik Torun, Hali̇l İbrahi̇m Gündüz, Osman Oktar, Cezmi̇ Türkmen, Efdal Kaya
Turkish Journal of Earth Sciences
The Tuz Gölü Fault Zone (TGFZ) is one of the most important active tectonic structures of Central Anatolia. The morphotectonic features of the TGFZ and the distribution of the epicenters of earthquakes over magnitude 5.0 show that this fault zone remains active today. In this study, the deformation of the TGFZ is determined with high sensitivity using geodetic measurements. To obtain accurate information about the deformation of the TGFZ, 24 GNSS sites and two continuously operating reference stations were constructed in the southern part of the TGFZ. Between 2018 and 2020, Global Navigation Satellite Systems (GNSS) measurements were made on …
Tectonic And Structural Characteristics Of Erzurum And Its Surroundings(Eastern Turkey): A Detailed Comparison Between Different Geophysical Parameters, Çağlar Özer, Serkan Öztürk, Eren Pamuk
Tectonic And Structural Characteristics Of Erzurum And Its Surroundings(Eastern Turkey): A Detailed Comparison Between Different Geophysical Parameters, Çağlar Özer, Serkan Öztürk, Eren Pamuk
Turkish Journal of Earth Sciences
The tectonic and structural properties of Erzurum and its surroundings have been investigated by evaluating the seismotectonic b - value, magnetic anomaly, edge detection analysis (total horizontal derivative (THDR) and tilt angle (TA)), Curie Point Depth (CPD), P-wave velocity (Vp), and Vp / Vs (S - wave velocity) ratio and by imaging the regional distributions of these parameters. For this purpose, all parameters have been combined to be able to reveal the new useful results on the study region and are presented for different locations and depths. The Vp values have been accompanied by high Vp / Vs ratios and …
Overview On Gplates: Focus On Plate Reconstruction, Shatavisa Chatterjee, Soumyajit Mukherjee
Overview On Gplates: Focus On Plate Reconstruction, Shatavisa Chatterjee, Soumyajit Mukherjee
Turkish Journal of Earth Sciences
Plate tectonic reconstructions have been employed in geosciences since 1970s, in the context of hydrocarbon exploration, regional geology and paleobiology. Such studies have given valuable inputs for climate and geodynamic computations, present-day mantle structure, models of plate motion, and the interpretation of the drift of hotspots, true polar wander (TPW), sea level and stratigraphic signals. However, geodynamic models generated in the past by incorporating global plate tectonic reconstructions have limitations. To overcome this, GPlates software brings forward a new era of interactive plate tectonic reconstruction software integrated with GIS databases that incorporates a wide variety of geological and geophysical data. …
Mineralogical, Petrological, And Geochemical Characteristics Of Şenkaya Chrysoprase,Turkey, Hami̇t Haluk Seli̇m, Aykut Güçteki̇n, Ferhan Şahi̇n, Mustafa Kaya, Beri̇l Kaya, Elanur Güner, Kami̇l Ömer Taş, Ahmet Karakaş, Yasemi̇n Kantarçeken
Mineralogical, Petrological, And Geochemical Characteristics Of Şenkaya Chrysoprase,Turkey, Hami̇t Haluk Seli̇m, Aykut Güçteki̇n, Ferhan Şahi̇n, Mustafa Kaya, Beri̇l Kaya, Elanur Güner, Kami̇l Ömer Taş, Ahmet Karakaş, Yasemi̇n Kantarçeken
Turkish Journal of Earth Sciences
Şenkaya chrysoprase is a gemstone and can be found near the Turnalı village located in the west-northwest of Şenkaya (Erzurum) county in the uplifted Kırdağ of Northeast Anatolia of Turkey. Chrysoprase only found in Şenkaya County and known with the same name commercially in Turkey is a light-dark green and cryptocrystalline structure gemstone encountered in the Örükyayla Mélange. Samples were collected from the field for defining mineralogical-petrographical, XRD, XRF, ICP-MS, optical cathodoluminescence microscopy (OCLM), FTIR-Raman and stable isotopic properties of Şenkaya chrysoprase. According to mineralogical and petrographic examination, Şenkaya chrysoprase has generally heterogeneous color distribution in macroscale and has 5 …
Hydrochemical Characteristics And Geothermometry Applications Of Thermal Waters Inthe Çürüksu Graben, Western Turkey, Ali̇ Gökgöz, Hali̇m Mutlu, Mehmet Ali̇ Akman
Hydrochemical Characteristics And Geothermometry Applications Of Thermal Waters Inthe Çürüksu Graben, Western Turkey, Ali̇ Gökgöz, Hali̇m Mutlu, Mehmet Ali̇ Akman
Turkish Journal of Earth Sciences
In this study, we investigate chemical and isotopic characteristics of low-temperature geothermal waters issuing from carbonate reservoirs in the Çürüksu Graben within the eastern termination of the Büyük Menderes Graben in western Turkey. Temperatures and pH values of geothermal waters vary from 20.1 to 24.6 °C and 6.62 to 7.11 and those of cold waters are 17.1 to 19.9 °C and 6.85 to 7.72, respectively. Geothermal waters are of Ca-HCO3 and Ca-SO4 types whereas cold waters are characterized by these two types and Mg-HCO3 as well. δ18O and δD values of samples vary from ?9.27‰ to -7.69‰ (VSMOW) and -58.06‰ …
Walkaway Vertical Seismic Profiling (Wvsp) Modeling And Imaging Study Along Faultedcoal Seams Over A High Velocity Limestone Model: A Synthetic Study, Cemal Erdemi̇r
Turkish Journal of Earth Sciences
The problem of collecting reflection data from the layers below a high velocity layer (HVL) and imaging those layers accurately is solved using walkaway vertical seismic profiling (WVSP) technique. The procedure is shown on a dataset from a model of highly faulted, thin-bedded coal layers separated by a high velocity layer of limestone. By locating the receivers above, in, and below the HVL, the reflections are expected to be recorded locally in situ in the borehole below the HVL before they travel back to the surface as in the case of surface seismic. The imaging results obtained from the model …
Detrital Composition Of Triassic To Neogene Sandstones In The Sulaiman Fold-Thrust Belt, Pakistan: Implications For Pre- And Postcollisional Evolution Of The Northwestern Indian Margin, Shazia Fareed, Akhtar Kassi, Aimal Kasi, Namik Aysal
Detrital Composition Of Triassic To Neogene Sandstones In The Sulaiman Fold-Thrust Belt, Pakistan: Implications For Pre- And Postcollisional Evolution Of The Northwestern Indian Margin, Shazia Fareed, Akhtar Kassi, Aimal Kasi, Namik Aysal
Turkish Journal of Earth Sciences
Sandstones of the Triassic through Pliocene successions of the western Sulaiman Fold-Thrust Belt (SFTB), Pakistan, were studied, by polarizing microscope and using point-counting techniques, to determine systematic variations in detrital modes. The sandstones in the study area are categorized into pre- and postcollisional sandstone assemblages. The precollisional assemblage was deposited before the onset of collision of India with Eurasia (starting Late Cretaceous-Early Paleocene) and subcategorized as Wulgai- Mughal Kot, Bibai and Pab subassemblages. The postcollisional assemblage was deposited after the onset of collision and categorized as Ghazij and Urak subassemblages. The Wulgai-Mughal Kot subassemblage mostly comprises of highly quartzose sandstones …
Relative Tectonic Activity Assessment Of Kütahya Graben (Western Anatolia): Insights From Geomorphic Indices, Zeynep Kezer, Erman Özsayin
Relative Tectonic Activity Assessment Of Kütahya Graben (Western Anatolia): Insights From Geomorphic Indices, Zeynep Kezer, Erman Özsayin
Turkish Journal of Earth Sciences
Western Anatolia is known as one of the most seismically active regions in the world, consistent with earthquakes having a magnitude >6.0. The deformation in the region is predominantly controlled by normal faults, which play significant role on the morphological features as well as depositional processes in related grabens. WNW-trending Kütahya Graben is located at the northeastern part of this province and bounded by several N- and S-dipping active normal fault segments. This study aims to investigate the relative tectonic activity among the fault segments of the Kütahya Graben using geomorphic indices. The analyses of this study include mountain-front sinuosity …
Late Ediacaran Inertial-Interchange True Polar Wander (Iitpw) Event: A New Road To Reconcile The Enigmatic Paleogeography Prior To The Final Assembly Of Gondwana, Bin Wen, Cairong Luo, Yong-Xiang Li, Yanting Lin
Late Ediacaran Inertial-Interchange True Polar Wander (Iitpw) Event: A New Road To Reconcile The Enigmatic Paleogeography Prior To The Final Assembly Of Gondwana, Bin Wen, Cairong Luo, Yong-Xiang Li, Yanting Lin
Turkish Journal of Earth Sciences
The Ediacaran to Early Cambrian plate tectonics was dominated by a full dispersal of the supercontinent Rodinia and the subsequent amalgamation of Gondwana. There is a consensus that the final assembly of Gondwana was not completed until the Early Cambrian. Prior to the final assembly, however, one major uncertainty remains on the quantitative paleogeography: the mainland of Gondwana was plausibly positioned at either a high or low latitude at a single time instant to meet the dual-latitude ('high-latitude' and 'low-latitude') options of Laurentia and the requirement of
A Preliminary Account On Devonian Trilobites From Arabian Plate, Se Turkey, Catherine Cronier, İzzet Hoşgör
A Preliminary Account On Devonian Trilobites From Arabian Plate, Se Turkey, Catherine Cronier, İzzet Hoşgör
Turkish Journal of Earth Sciences
Recently, several Devonian localities and the related biota occurring from the southeastern Turkey were reinvestigated. Although, the Hakkari-Çukurca and the Diyarbakır-Hazro areas of the Arabian Plate are considered as an important source of the Devonian macrofossils from the north Arabian sector of Gondwana, the existing record of Devonian trilobites in these regions was hitherto unknown. We here report and illustrate for the first time Lower and Middle Devonian trilobites represented by three proetid pygidia and one calymenid pygidium. The morphological features of these pygidia suggest that they can be assigned to undetermined species of Gravicalymene (Calymenidae) and Podoliproetus (Proetidae), two …
Nature And Crystallization Stages Of Spherulites Within The Obsidian: Acıgöl (Cappadocia- Nevşehir, Turkey), Bahatti̇n Güllü, Kiymet Deni̇z
Nature And Crystallization Stages Of Spherulites Within The Obsidian: Acıgöl (Cappadocia- Nevşehir, Turkey), Bahatti̇n Güllü, Kiymet Deni̇z
Turkish Journal of Earth Sciences
The study area comprises a part of the Central Anatolian Cenozoic volcanism within the Cappadocia Volcanic Province (CVP). Obsidian, perlite rhyolite flows, and volcanic ashes are observed in the study area and the spherulites within the obsidian are the objects of this study. The spherulites occupied within the obsidian in the form of round nodules 0.5-10 cm in diameter. The confocal Raman spectra of feldspar minerals within the spherulites are characterized by T-O-T and M-O lattice modes in the range of 100-250 cm-1, O-T-O deformation and T-O-T lattice modes in the range of 250-350 cm-1, and …
Analysis, Processing, And Migration Of The Marine 4-Component Walkaway Vsp Data Set From The Seg Seam-1 Gulf Of Mexico Salt Elastic Modelling Project: Synthetic Study, Cemal Erdemi̇r
Turkish Journal of Earth Sciences
The four component (4C) walkaway vertical seismic profile (WVSP) marine elastic synthetic data set from the SEG's SEAM-1 salt modeling project in the Gulf of Mexico (GOM) are examined, analyzed, processed, and migrated for P-P reflections using a reverse time prestack migration (RTM) algorithm to construct a subsurface image around the Well-1 VSP borehole. The imaging results from the three data sets; pressure-p, geophone vertical (z), and horizontal inline (x) components, have shown great successes in correctly locating and imaging sediments near and below the borehole as well as the vertical face of the salt, which is about 5 km …
Vertical Variations Of Minerals In Clayey Sedimentary Rocks In The Cores Of Two-Deep Exploration Wells From The Kozlu Coalfield (Zonguldak, Nw Türkiye), With Emphasis On Tonstein (Schieferton) Formation, Ali̇ İhsan Karayi̇ği̇t, Emi̇ne Sütcü, Abi̇di̇n Temel, Mustafa Ni̇yazi̇ Gündoğdu
Vertical Variations Of Minerals In Clayey Sedimentary Rocks In The Cores Of Two-Deep Exploration Wells From The Kozlu Coalfield (Zonguldak, Nw Türkiye), With Emphasis On Tonstein (Schieferton) Formation, Ali̇ İhsan Karayi̇ği̇t, Emi̇ne Sütcü, Abi̇di̇n Temel, Mustafa Ni̇yazi̇ Gündoğdu
Turkish Journal of Earth Sciences
The majority of Turkish bituminous coal resources are located in the Zonguldak Basin. The Carboniferous coal seams in the Alacaağzı, Kozlu, and Karadon formations have received interest. However, the detailed mineralogical compositions of clayey sedimentary rocks in coal-bearing sequences in the basin have been limited. This study aims to investigate vertical variations of mineralogical compositions of Carboniferous and Early Cretaceous clayey sedimentary rocks cored in the two-deep exploration wells (K20/K and K20/H) from the Kozlu coalfield using XRD and SEM-EDX analyses data. In addition, a special interest is also given to tonstein layers identified within the Kozlu and Karadon formations. …
Detection And Interpretation Of Precursory Magnetic Signals Preceding October 30, 2020 Samos Earthquake, İlki̇n Özsöz, Oya Ankaya Pamukçu
Detection And Interpretation Of Precursory Magnetic Signals Preceding October 30, 2020 Samos Earthquake, İlki̇n Özsöz, Oya Ankaya Pamukçu
Turkish Journal of Earth Sciences
A major earthquake (Mw=7.0) occurred in the Samos Island on the 30th of October 2020 at 11:51 UTC. Swarm satellite magnetic data were analysed for 153 days before and 46 days after the earthquake. Preearthquake and postearthquake anomaly search is constrained within the Dobrovolsky's Circular Area. Fundamentally, there are 5 steps for processing satellite magnetic data to interpret the earthquake preparation phase. The first step is converting geographical coordinates to geomagnetic latitude and longitude. Secondly, intensity of the external magnetic field should be evaluated by magnetic indices (Ap, Kp and Dst). Thirdly, preearthquake and postearthquake magnetic anomaly should be constrained …
Seismic A And B-Values And Crustal Parameters Of Samos Island-Aegean Sea, Lesvosisland-Karaburun, Kos Island-Gökova Bay Earthquakes, Oya Pamukçu, Fi̇kret Doğru, Ayça Çirmik, Düzgün Göneş
Seismic A And B-Values And Crustal Parameters Of Samos Island-Aegean Sea, Lesvosisland-Karaburun, Kos Island-Gökova Bay Earthquakes, Oya Pamukçu, Fi̇kret Doğru, Ayça Çirmik, Düzgün Göneş
Turkish Journal of Earth Sciences
In recent years, seismicity has increased considerably in the Aegean Sea region and there have been earthquakes in which people lost their lives. The major earthquakes, Kos Island-Gökova Bay (Mw = 6.6), Lesvos Island-Karaburun (İzmir) (Mw = 6.2) and Samos Island-Aegean Sea (Mw = 6.9) occurred in the Aegean Sea and affected Aegean region strongly. Within the scope of this study, the seismic b-value of these major earthquakes was calculated in order to perform earthquake statistical analysis. Seismic a and b-values within the first 24 h and 14 days after the mainshock determination of Kos Island-Gökova Bay, Lesvos Island-Karaburun (İzmir) …
Fault-Controlled Gas Escapes In The Shelf Sediments Of The Saros Gulf, Ne Aegean Sea, Şebnem Önder, Naci̇ Görür, Alina Polonia, Luca Gasperini
Fault-Controlled Gas Escapes In The Shelf Sediments Of The Saros Gulf, Ne Aegean Sea, Şebnem Önder, Naci̇ Görür, Alina Polonia, Luca Gasperini
Turkish Journal of Earth Sciences
High-resolution marine seismic reflection studies on the eastern shelf of the Saros Gulf have revealed the presence of gas-charged sediments across a narrow submarine valley incised by the Ganos Fault along the North Anatolian Fault system. Quaternary sediments, accumulated during glacial and interglacial periods through transgressional and progradational units, were controlled by glacio-eustatic sea-level fluctuations and tectonic deformation. The transgressional units made of upward-fining deposits created seals at their tops to form gas accumulation pockets. Conversely, the progradational units appear heavily eroded at their top, which is unfavorable for gas accumulation. The sediment?s gas accumulation features include enhanced reflections, acoustic …
Hydrogeochemical Fingerprints Of A Mixohaline Wetland In The Mediterranean: Güllük Coastal Wetland Systems- Gcws (Muğla, Turkey), Adi̇le Meli̇s Somay Altaş
Hydrogeochemical Fingerprints Of A Mixohaline Wetland In The Mediterranean: Güllük Coastal Wetland Systems- Gcws (Muğla, Turkey), Adi̇le Meli̇s Somay Altaş
Turkish Journal of Earth Sciences
The Güllük coastal wetland system (GCWS), which is located at the contact point of the Menderes Massif and Lycian Nappe, consists of both brackish karstic [Güllük Lagoon wetland (GLW)] and saline [Boğaziçi-Tuzla (Bargylia) coastal wetland (BTW)] ecosystems in western Turkey, and is under protection as a national wetland of importance. This area is important for its unique wetland features, aquaculture, tourism, agriculture, Bodrum airport, and Güllük port facilities. The aim of this study was to evaluate the GLW and BTW, both hydrogeologically and hydrogeochemically, for the first time together. The mixohaline GCWS is recharged from precipitation, streams, and brackish karstic …