Browsing by Author "Turgut S."

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    Sequence stratigraphy, tectonics and depositional history in eastern Thrace Basin, NW Turkey
    (2000) Turgut S.; Eseller G.
    The eastern Thrace Basin forms the eastern portion of the Turkish Thrace Basin in NW Turkey. The pre-Tertiary crystalline basement shows platform and deep basin depositional morphology which results in facies pattern and thickness distribution localization during the early stages of basin development in Middle to Late Eocene time. Normal fault controlled early and lateral/reverse fault controlled later stage tectonic events characterize basin geometry and the present topography, respectively. The early stage normal faulting caused subsidence and sediment accumulation in the Late Eocene and Early Oligocene, while later stage tectonic events caused intense deformation and structuration in the Early to Middle Miocene. As a result, southeastern and northern regions were folded or uplifted and deeply eroded. Outcrop, well log, core and reflection seismic studies reveal that the sedimentary succession can be subdivided into five characteristic depositional sequences bounded at their base by unconformities. These unconformities were dated using paleontological data. The sequence boundaries, underlying consecutively Sequences-1, 2, 3, and 5 were dated at 39.5, 36, 30, and 25.5 Ma from older to young in order of succession, corresponding to the major erosional breaks between the Middle and Upper Eocene, the Upper Eocene and the Lower Oligocene, the Lower and Upper Oligocene, and the Upper Oligocene and the Lower Miocene. The sequence boundary underlying Sequence-4 was determined to lie within the Late Oligocene succession and, as an age designation could not be assigned, it was termed intra sequence boundary (ISB). The first two sequences correspond to relative sea level rises and a normal fault controlled tectonism coincides with them. Reefal carbonates, coarse grained clastics and marine shales, with abundant volcanic flows or layers represent the sedimentary facies of these two early sequences. The third and fourth sequences correspond to either a decreased relative rise of sea level or a relative still stand of sea level and a sediment-induced subsidence related to thermal relaxation provides accommodation. Prograding delta sediments of varying extent constitute the sedimentary packages of these two sequences. The Depositional Sequence-5, which makes up the uppermost part of the sedimentary succession in the basin, corresponds to a relative sea level fall and a tectonic style shaped by lateral and inversion faulting characterizes this period. Nonmarine alluvial fan, fluvial channel and various lagoonal deposits constitute the sedimentary facies of this last sequence. Porous reefal limestones and shallow marine beach sandstones of Sequence-1 and deltaic sandstones of Sequences-3 and 4 provide good reservoir rocks for the hydrocarbons produced in the study area. The marine shales and marls of the second and the third sequences provide good source rocks as they are rich in disseminated organic matter content. Although the non-marine alluvial and fluvial channel deposits of Sequence-5 are good reservoirs, they lack effective seals. The time interval in which Sequence-5 was deposited represents a period of major structural and trap development in the basin. (C) 2000 Elsevier Science Ltd. All rights reserved.; The eastern Thrace Basin forms the eastern portion of the Turkish Trace Basin ni NW Turkey. The pre-Tertiary crystalline basement shows platform and deep basin depositional morphology which results in facies pattern and thickness distribution localization during the early stages of basin development in Middle to late Eocene time. Normal fault-controlled-early and lateral/reverse fault-controlled-later stage tectonic events characterized basin geometry and the present topography, respectively. The early stage normal faulting caused subsidence and sediment accumulation in the Late Eocene and Early Oligocene, while later stage tectonic events caused intense deformation and structuration in the Early to Middle Miocene.
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    Figure of merit of one-dimensional resonant transmission systems in the quantum regime
    (Association for Scientific Research, 2009) Ç̧ipiloǧlu M.A.; Turgut S.
    The figure of merit, ZT, for a one-dimensional conductor displaying a Lorentzian resonant transmission probability is calculated. The optimum working conditions for largest ZT values are determined. It is found that, the resonance energy has to be adjusted to be several resonance widths away from the Fermi level. Similarly it is better for the temperature to be equal to several resonance widths. The approximate relationships, which can be a fairly good guide for designing devices, between different parameters under optimum working conditions are given. © Association for Scientific Research.
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    Comparison of clinical, hormonal, pathological and treatment outcomes of ectopic Cushing’s syndrome by sex: results of a multicenter study
    (Springer, 2024) Ciftci S.; Yilmaz N.; Selcukbiricik O.S.; Hekimsoy Z.; Canpolat A.G.; Topsakal S.; Yaylali G.F.; Misiroglu F.; Gul N.; Uzum A.K.; Hacioglu A.; Yorulmaz G.; Ozisik H.; Yurekli B.S.; Pekkolay Z.; Turgut S.; Karaca Z.; Duran C.; Kebapci M.N.; Yarman S.
    Objective: To compare clinical and hormonal data, neuroendocrine neoplasia (NEN) localization, treatment, and survival outcomes in ectopic Cushing’s syndrome (ECS) by sex. Methods: Eleven experienced centers from our country participated in this retrospective study. The clinical and hormonal features, tumor imaging, pathological results, treatment modalities, and disease courses of the patients were evaluated. Results: 28 female and 26 male patients with ECS were compared. The mean age at diagnosis, clinical characteristics, and hormonal evaluation results were similar. However, insulin-requiring diabetes mellitus (p = 0.04) and osteoporosis with fractures were more common in males (p = 0.03). While more patients with increased DHEA-S levels than the upper limit of normal were found to be higher in females, central hypothyroidism were higher in males (p = 0.02). At the diagnosis, 36 NENs (68% of females and 69% of males) were localized. Small cell lung carcinoma was higher in males (p = 0.02), and the frequency of other NENs was not different. Curative surgery was performed on 61% of females and 46% of males. Tumor size, Ki-67 labeling index, positive ACTH immunostaining, local lymph node and distant metastasis rates were similar in both sexes. In the follow-up, the tumor became visible in 7 of 10 females and 4 of 8 males after medical treatment and/or bilateral adrenalectomy. The remission rates (65% of females, 62% of males) and NEN-related death rates (14% of females, 30% of males) were similar. Conclusion: While ECS has a similar disease course in many aspects in males and females, hyperglycemia and osteoporosis are more severe in males. © The Author(s), under exclusive licence to Springer Science+Business Media, LLC, part of Springer Nature 2024.